10001 adcp adcp http://globec.whoi.edu/jg/serv/globec/gb/adcp.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/adcp%7D <center><h2>Acoustic Doppler Current Profiler Data </h2></center> ADCP data from the U.S. GLOBEC Georges Bank Program are available from a web site maintained by Dr. Charles Flagg presently located at SUNY Stony Brook. <p> Data are retrieved by cruise directly from the database via user supplied selection criteria. The data are returned in either .mat file or plain ASCII files. Output includes yearday, lon, lat, depth(m), u(m/s), v(m/s), backscatter intensity, estimated zooplankton biomass, water temp, and water depth. <p>The web-page contains the results of the shipboard ADCP data collection effort for GLOBEC's Georges Bank Project. The ADCP data has been acquired onboard the RV Endeavor, the RV Oceanus, the Edwin Link, and the Albatross IV for each GLOBEC cruise. At the end of each cruise the pingdata files are sent to us for processing. The vast majority of the data has been collected using 150 kHz narrow-band ADCPs although there have been a number of cruises on the RV Albatross which is equipped with a broad-band unit. Recently, we have completed the modification and development of the routines required to deal with the broad-band data and those cruises are now being gradually included in the ADCP archive. <p>The ADCP data are processed using the CODAS3 shipboard ADCP processing programs developed by the University of Hawaii with additional capabilities developed at Brookhaven. As the data from each cruise is processed, it is made accessible through this web page which allows for the downloading of user specified portions from each cruise in either flat-ASCII or mat file formats. Cruise plots are available for viewing which show the spatial extent of the data coverage for each cruise. The broadscale cruises typically provide the widest coverage although some of the process cruises have excellent coverage in limited areas. <p>The assistance of Bill Fanning, Jim Akens, Laura Goepfert, Melissa Lamont, and Jim Manning in overseeing the shipboard collection and forwarding of the ADCP data to BNL is gratefully acknowledged. <p>As part of the analysis of the ADCP data set, we have embarked upon a hindcast modelling effort based upon the work of the Dartmouth/UNC/WHOI/NMFS/BIO/BNL realtime modelling program. The goal is to provide realistic spatial and temporal interpolations of the ADCP currents over the Bank for as many cruises as possible in order to study the large-scale mean and seasonal flow patterns. The hindcast process uses a fully non-linear forward model and a variety of linearized inverse models in an iterative procedure to capture as much of the observed variability in the ADCP data as possible. The resulting model fields then provide a reasonable spatial and temporal prediction of the currents and property distributions over the Bank during the cruise period. Results from the hindcast modelling are also being made accessible through this web site as they become available. The basic results of the model come in the form of hourly barotropic currents and sea-level and complete 3-D results for the model domain at six-hourl y intervals. The current version of the hindcast model uses the Bank150 grid, a map of which can be viewed by clicking here. The invaluable assistance of Chris Naimie, Jim Manning and Brian Blanton in setting this program up is much appreciated. <p>* PLEASE NOTE: A minor calibration error was detected and corrected. All of the necessary corrections were performed between 7/28/00 to 10/3/00. <p>* Due to an erroneous dip switch toggle on the Endeavor ADCP (discovered by Jules Hummond and Daryl Symonds), the 1999 Endeavor ADCP data contained errors. The errant profiles (approx 2%) were removed and affected datasets completely reprocesses on 3/12/01. <pre> Questions regarding these data should be directed to: Dr. Charles Flagg Marine Science Research Center Stony Brook University Stony Brook, NY 11794-5000 PHONE:(631) 632-3184 FAX: (631) 632-8820 EMAIL:<a href="mailto:cflagg@ms.cc.sunysb.edu">cflagg@ms.cc.sunysb.edu</a> or Maureen Dunn <a href="mailto:maudunn@notes.cc.sunysb.edu">maudunn@notes.cc.sunysb.edu </a> Marine Science Research Center Stony Brook University, NY 11794-5000 <i>Last update: December 12, 2006 </i> </pre> The ADCP data has been acquired onboard the RV Endeavor, the RV Oceanus, the Edwin Link, and the Albatross IV for each GLOBEC cruise. At the end of each cruise the pingdata files are sent to us for processing. The vast majority of the data has been collected using 150 kHz narrow-band ADCPs although there have been a number of cruises on the RV Albatross which is equipped with a broad-band unit. The ADCP data are processed using the CODAS3 shipboard ADCP processing programs developed by the University of Hawaii with additional capabilities developed at Brookhaven. 10002 all_species_seen all_species_seen http://globec.whoi.edu/jg/serv/globec/gb/all_species_seen.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/all_species_seen%7D <b>Contributed by:</b> Maria Casas and Ted Durbin <p> <b>Date:</b> February 13, 2004</p><p> This data object shows <b>all</b> the species identified during the US GLOBEC Georges Bank broad-scale cruises, including MOC and Pump instruments. This list will be used by the Zooplankton meter² count data from GSO/URI and the Zooplankton meter³ count data from GSO/URI data objects to help define which species were expected to be found. 10003 bathymetry bathymetry http://globec.whoi.edu/jg/serv/globec/gb/bathymetry.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/bathymetry%7D <center><h2>Georges Bank Gridded Bathymetry</h2></center> <b>Contributor:</b><br> Dave Greenberg<br> Bedford Institute of Oceanography <br> Dartmouth, Nova Scotia<br> Canada</p> <p>Julio Candela<br> Woods Hole Oceanographic Institution<br> Prepared data for on-line use</p> <p><i>Updated: December 08 2004; <br> GHeimerdinger</i> 10004 bathy_ADCP bathy_ADCP http://globec.whoi.edu/jg/ <center><h2>Georges Bank bathymetry from ADCP data </h2></center> <p><b>DMO note:</b><br> Year of data can be obtained from cruise report(s).</p> <p><b>Contributor:</b><br> Charles Flagg,<br> Endeavour Hall, Rm 203<br> Marine Science Research Center<br> SUNY Stony Brook<br> Stony Brook, NY 11794<br> <a href="mailto:cflagg@mc.cc.sunysb.edu">cflagg@mc.cc.sunysb.edu</a><br> </p><p>Julio Candela prepared the data for on-line use.</p> <p><i>last update: March 13, 2006.</i></p> Georges Bank bathymetry from the ADCP Endeavor data from Charles Flagg, Brookhaven National Laboratories 10005 BMP2_ess BMP2_ess http://globec.whoi.edu/jg/serv/globec/gb/BMP2_ess.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/BMP2_ess%7D <center><h2>Georges Bank BIOMAPERII Environmental (CTD+) Data </h2></center> <p>These data are from the Enviromental Sensing System (ESS) part of the <u>BIO</u>-Optical <u>M</u>ulti-frequency <u>A</u>coustical and <u>P</u>hysical <u>E</u>nvironmental <u>R</u>ecorder or BIOMAPER II¹.</p> <p>"The system consists of a multi-frequency sonar (up-looking and down-looking pairs of transducers operating at five frequencies: 43,120,200,420, and 1000kHz), a video plankton recorder system (VPR), an environmental sensor system (CTD, fluorometer, transmissometer), and several other bio-optical sensors (down- and upwelling spectral radiometers, spectral attenuation, and backscattering, and absorption meters)."¹</p> <h2>References</h2> ¹Wiebe, P.H., et al., 2002, BIOMAPER-II: An Integrated Instrument Platform for Coupled Biological and Physical Measurements in Coastal and Oceanic Regimes. IEEE Journal of Oceanic Engineering, <b>27(3)</b>:700-716.<p></p> <p>²Fofonoff and Millard, 1983, UNESCO technical papers in Marine Sciences, #44</p> <b>Data Submitted by:</b> <p> <b> Data Submitted by:</b><br> <br> Peter Wiebe<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543 <br> voice: (508) 289-2313 <br> fax: (508) 457-2169 <br> <a href="mailto:pwiebe@whoi.edu">pwiebe@whoi.edu</a> </p> <i> updated November 15, 2005; gfh</i> </pre> These data are from the Enviromental Sensing System (ESS) part of the<u>BIO</u>-Optical <u>M</u>ulti-frequency <u>A</u>coustical and <u>P</u>hysical <u>E</u>nvironmental <u>R</u>ecorder or BIOMAPER II. 10006 broadscale_grid broadscale_grid http://globec.whoi.edu/jg/serv/globec/gb/broadscale_grid.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/broadscale_grid%7D The Broad-scale grid is defined by the points within this data file. It is used for Broad-scale gridding applications. Each rectangle in the grid is 0.05 degrees latitude by 0.05 degrees longitude. The area is the area, in km², that the grid point represents. The field names are as follows: <p> For information relating to the development of the grid, see the <a href="http://globec.whoi.edu/globec-dir/phase4doc/grid/grid_report.html"> Grid Report</a> </p><p> This is an example of a gridding <a href="http://globec.whoi.edu/globec-dir/data_doc/Broadscalegrid.html">datasheet</a>. <br> Download <a href="http://globec.whoi.edu/globec-dir/data_doc/BroadscaleGridData.xls">Excel</a> File. (Hold SHIFT key and Click to download)</p> <p><font color="red">Note:</font> Subregion 5 (<font color="blue">Slope Water</font>) has been redefined to include those points formerly in Subregion 3 (<font color="purple">Northeast Peak</font>) where the water is deeper than 150 meters.</p> <p><a href="http://globec.whoi.edu/images/bs-grid.html"> <img src="http://globec.whoi.edu/images/bsgridRevsm.jpg" alt="Broad-scale grid"></a> </p> <i>Last modified: June 16, 2004</i> 10007 broadscale_summary broadscale_summary http://globec.whoi.edu/jg/serv/globec/gb/modeling/broadscale_summary.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/broadscale_summary%7D Thumbnail images of the broad-scale data, processed using kriging techniques, are displayed here. Clicking on the thumbnail image will open a new browser window displaying the original, large image. Matlab data files are also accessible on these pages by clicking on the appropriate link. Matlab data files are of kriged values for Georges Bank with 2385 grid points. Note that on some browsers it will be necessary to hold down the "shift key" before clicking on the link in order to download the data to a file. Otherwise the data are loaded into your browser. Unless your browser knows what to do with Matlab binary data, it is best to download the whole file. <p> Thumbnail images were created from the original Matlab generated images using the mogrify utility in a single batch operation prior to serving. The thumbnail image page, however, is created each time it is viewed so that the most recent images are incorporated in the served data. </p><p> These maps were created using EasyKrig 3.0 (D. Chu, WHOI, 2004, <a href="http://globec.whoi.edu/software/kriging/easy_krig/easy_krig.html" target="_blank"> http://globec.whoi.edu/software/kriging/easy_krig/easy_krig.html</a>.) All data were treated anisotropically, i.e., the variable of interest changes more rapidly in one direction than in another, essentially stretching the effect. In this case the x:y ratio was 2:1 and the rotation was 45 degrees for alignment with the Bank. These parameters were chosen based upon known circulation and geography of Georges Bank. When plotting the station locations as circles on the maps, only those stations containing data are shown. Some datasets are quite sparse, e.g. ammonia at 50-100m. <p> <b>Nutrients:</b> nitrates & nitrites (NO3/NO2), ammonia (NH4), silica (SiOH4), phosphates (PO4) (Townsend et al, U. Maine):<br> Data are available for 1997-1999, for January through June except:<br> </p><dir> 1997: no January or June<br> 1998: no January </dir> <p> The same colorbar range was used for the nutrient maps (nitrates/nitrites, ammonia, phosphates, silicates) as D. Townsend used in his plots, located on the GLOBEC website at: <a href="http://globec.whoi.edu/jg/info/globec/gb/nut_phyto%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,data=grampus.umeoce.maine.edu/jg/serv/globec/nut_phyto.html0%7D?" target="_blank"> http://globec.whoi.edu/jg/info/globec/gb/nut_phyto%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,data=grampus.umeoce.maine.edu/jg/serv/globec/nut_phyto.html0%7D?</a> </p><p> Chlorophyll-a values for 1995-1996 (February through July "95 and January through June "96) are from the ctd_hydrography; the 1997-1999 data are from D. Townsend"s nutrient data. The color range is given as both 0-6 and 0-10 in order to make both large and small scale variations more clearly visible. </p><p> Nutrient and chl-a data were averaged from 3 depth strata: 0-15m, 15-50m, and 50-100m. There were usually one or two bottle samples in each range. </p><p> Biovolume data from bongo net displacement volumes is from D. Mountain, Jack Green and Joe Kane, NMFS: <a href="http://globec.whoi.edu/jg/serv/globec/gb/broadscale/bongovols.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/bongovols%7D" target="_blank"> http://globec.whoi.edu/jg/serv/globec/gb/broadscale/bongovols.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/bongovols%7D</a> </p><p> Temperature, fluorometry, salinity and density stratification values were kriged from data provided by D. Mountain at <a href="http://globec.whoi.edu/jg/dir/globec/gb/broadscale/" target="_blank"> http://globec.whoi.edu/jg/dir/globec/gb/broadscale/</a> under ctd_hydrography. </p><p> The density stratification was calculated by first finding the density of each station and depth for which there was a temperature and salinity using a Matlab mfile function called <a href="http://usjgofs.whoi.edu/globec-dir/software/sw_dens.m" target="_blank">sw_dens.m</a>. Then the mean density was calculated for the depth strata 0-15 meters and for 50-100 m. If the maximum depth of a station was less than 50 m, the mean of 25-50m was used as the deep value. The difference is the stratification index. </p><p> </p><h4>VARIABLE STRUCTURE</h4> There are two structures: "para" and "data", where structure "para" contains all parameters including "load data", "variogram", "kriging", and "display", and structure "data" contains the input ("in") and output data ("out") structures. <p> </p><pre>1. PARAMETERS VARIABLE NAME DESCRIPTION para Parameters Structure .home_dir home directory .optim flag of optimization tool box .dataprep Data Preparation parameters .filename input filename .fileID File ID for the data set .x_norm normalization factor for variable 1 .y_norm normalization factor for variable 2 .z_norm normalization factor for variable 3 .x_offset coordinate offset for variable 1 .y_offset coordinate offset for variable 2 .z_offset coordinate offset for variable 3 .latlonfac conversion factor between longitude/latitude (deg) and x/y (length) .reduct_fac data reduction factor .filter_type filter type .filter_supt filter support .transform_index index of data transformation model .vario (Semi-)Variogram/Correlogram parameters .model model index of variogram/correlogram .sill sill .lscl relative length scale .nugt nugget .powr power .hole scale of hole effect .range range of modeling .res resolution of the lag .angle anisotrophy angle .ratio anasotrophy aspect ratio .ang_res angle resolution of 2D variogram/correlogram .para_file parameter filename .krig Kriging parameters .xmin minimum x-coordinate .xmax maximum x-coordinate .dx resolution in x direction .ymin minimum y-coordinate .ymax maximum y-coordinate .dy resolution in y direction .zmin minimum z-coordinate .zmax maximum z-coordinate .dz resolution in z direction .model kriging model index .scheme kriging scheme index .blk_nx horizontal block size (only for point-block kriging) .blk_ny vertical block size (only for point-block kriging) .srad kriging search radius .kmin minimum kriging points .kmax maximum kriging points .elim relative error limit .batch_file_proc flag for batch file processing .batch_data_file file that contains a list of input data filename(s) for batch processing .grid_file filepath and filename of the customized grid file 2. OUTPUT AND INPUT DATA VARIABLE NAME DESCRIPTION data Data Structure .in Input data .dim dimension of the input data .var1 x-coordinates of raw data after duplicated data and nan"s removed .var2 y-coordinates of raw data after duplicated data and nan"s removed .var3 z-coordinates of raw data after duplicated data and nan"s removed .var raw data after duplicated data and nan"s removed .x x - coordinates after initial manipulation (reduction, normalization) .y y - coordinates after initial manipulation (reduction, normalization) .z z - coordinates after initial manipulation (reduction, normalization) .v data after initial data processing (reduction) .tvar transformed data from data.in.var. .tv transformed data from data.in.v .out Output data .vario Data output from semi-variogram/correlogram computation .c0 variance .lag lag of semi-variogram (correlogram) .gammah semi-variogram .cnt count of data pairs at each lag .ang angle array for 2D semi-variogram/correlogram .x x-axis of 2D semi-variogram/correlogram .y y-axis of 2D semi-variogram/correlogram .lag_theo lag used in model-based variogram/correlogram .gammah_theo model-based semi-variogram .gammah2d 2D semi-variogram .krig Data output from kriging .nx output data dimension: nx * ny for 2D and nx * ny * nz for 3D .ny output data dimension: nx * ny for 2D and nx * ny * nz for 3D .nz output data dimension: nx * ny * nz for 3D .xg normalized grided x-coordinate .yg normalized grided y-coordinate .zg normalized grided z-coordinate .gx normalized grided x-coordinates for customized grids .gy normalized grided y-coordinates for customized grids .gz normalized grided z-coordinates for customized grids .Xg 2D/3D x-coordinate matrix .Yg 2D/3D y-coordinate matrix .Zg 3D z-coordinate matrix .Vg 2D/3D data from kriging at (Xg, Yg) .Eg 2D/3D kriging variance at (Xg,Yg) .Ig reshaped 1D representation of the 2D/3D variable Cg .eg reshaped 1D representation of the 2D/3D variable Eg .gv kriging results at the customized grids (gx, gy, gz) .ge kriging variance at the customized grids (gx, gy, gz) .Is predicted observed data from Double Kriging cross-validation .Ijk predicted observed data from leave-one-out cross-validation .ek normalized residual array in Q1 and Q2 cross-validations .q1 value of Q1 cross validation .q2 value of Q2 cross validation 3. Example To plot the kriging map using your own program, load the output file saved from easy_krig3.0 and then type: >>pcolor(data.out.krig.Xg,data.out.krig.Yg,data.out.krig.Cg); >>colorbar;shading interp to plot a kriging image, or >>pcolor(data.out.krig.Xg,data.out.krig.Yg,data.out.krig.Eg); >>colorbar;shading interp to plot the kriging variance image. The structured variable "data.out.krig.Xg" means "out" is a substructure under "data", "krig" is a substructure of "out", and "Xg" is a member (2d array) of the substructure "krig". All substructures and members of the primary structures "data" and "para" are listed and explained above (note that only part of those parameters may be useful to the users): </pre> <p> <i>Last modified: May 18, 2005</i> </p> 10008 chloro_bottle chloro_bottle http://globec.whoi.edu/jg/serv/globec/gb/chloro_bottle.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb /,info=globec.whoi.edu/jg/info/globec/gb/chloro_bottle%7D <h2 align=center> Raw Extracted Chlorophyll Data from <br> Broadscale CTD stations, 1995 and 1996.</h2> <p> <b> DMO NOTE:</b> <p> Latitude and Longitude positions for these stations can be merged into the file by using the JOIN 2 OBJECTS command under the Plotting and Other Operations button. From within the chloro_bottle object (data set) go to the Plotting and Other Operations at top of page. Under Manipulating data go to Join 2 objects. Click on US Globec Georges Bank. Follow instructions at top of page, in this case click on the object "eventlogs". Under the select only table, highlight cruiseid, cast, lat, and lon and click on continue. Click on Join. The merge is completed. </p> <b> PI NOTES:</b> <p>The 1995 and 1996 bottle data were collected with a GO rosette mounted above the MK5 CTD. Water for chlorophyll extractions was taken at priority 1 and 2 stations and at 3 "standard" depths (according to a protocal set up by Ted Durbin and Dian Gifford at the University of Rhode Island). For each bottle, 3 replicate samples were run for consistency. 50 mls were filtered for 3 size fractions: total chlorophyll, chlorophyll from water filtered through a &lt;20 micron mesh and chlorophyll from water filtered through a &lt;5 micron mesh. This means that for any one station, there were 27 test tubes: 3 depths, 3 replicates, 3 size fractions. The samples were usually read at sea (after the 24 hour acetone extraction). If not, Ted Durbin"s Lab read them when the ship returned.</p> <p> The companion object for this data is chloro_bot_chem, which details salinity, temperature, fluorometry and tranmissometry collected from the same bottles.</p> <hr> Contacts for the data:<br> <i>David Mountain<br> NMFS<br> Woods Hole, MA 02543 <br> 508-495-2271 <br> <a href="mailto:David.Mountain@noaa.gov">David.Mountain@noaa.gov</a><br> Fax: 508-495-2258<br></i> or<br> <i>Maureen Taylor<br> NOAA/NMFS <br> 166 Water Street <br> Woods Hole, MA 02543<br> 508-495-2306<br> <a href="mailto:mtaylor@whsun1.wh.whoi.edu">mtaylor@whsun1.wh.whoi.edu</a><br> FAX: 508-495-2258 </i></p> <i> Updated November 15, 2005; gfh </i> </pre> The 1995 and 1996 bottle data were collected with a GO rosette mounted above the MK5 CTD. Water for chlorophyll extractions was taken at priority 1 and 2 stations and at 3 &#039;standard&#039; depths (according to a protocal set up by Ted Durbin and Dian Gifford at the University of Rhode Island). For each bottle, 3 replicate samples were run for consistency. 50 mls were filtered for 3 size fractions: total chlorophyll, chlorophyll from water filtered through a <20 micron mesh and chlorophyll from water filtered through a <5 micron mesh. This means that for any one station, there were 27 test tubes: 3 depths, 3 replicates, 3 size fractions. The samples were usually read at sea (after the 24 hour acetone extraction). If not, Ted Durbin&#039;s Lab read them when the ship returned. 10009 chloro_bot_chem chloro_bot_chem http://globec.whoi.edu/jg/serv/globec/gb/chloro_bottle_chem.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/chloro_bot_chem%7D <h2 align=center> Water column properties, <br> Broadscale CTD stations, 1995 and 1996.</h2> <p> <b> DMO NOTE:</b> <p> Latitude and Longitude positions for these stations can be merged into the file by using the JOIN 2 OBJECTS command under the Plotting and Other Operations button. From within the chloro_bot_chem object (data set) go to the Plotting and Other Operations at top of page. Under Manipulating data go to Join 2 objects. Click on US Globec Georges Bank. Follow instructions at top of page, in this case, click on the object "eventlogs". Under select only table, highlight cruiseid, cast, lat, and lon and click on continue. Click on Join. The merge is completed and a new temporary file has been created. </p> <b> PI NOTES:</b> <p>The 1995 and 1996 bottle data were collected with a GO rosette mounted above the MK5 CTD. The temperature, conductivity, salinity, and fluorescence data were collected from the CTD data stream when the bottle was tripped (~30 scans are averaged).</p> <p> The companion object which includes the raw chlorophyll and phaeophytin values for these same cruises is chloro_bottle. </p> <hr> Contacts for the data:<br> <i>David Mountain<br> NMFS<br> Woods Hole, MA 02543 <br> 508-495-2271 <br> <a href="mailto:David.Mountain@noaa.gov">David.Mountain@noaa.gov</a><br> Fax: 508-495-2258<br></i> or<br> <i>Maureen Taylor<br> NOAA/NMFS <br> 166 Water Street <br> Woods Hole, MA 02543<br> 508-495-2306<br> <a href="mailto:mtaylor@whsun1.wh.whoi.edu">mtaylor@whsun1.wh.whoi.edu</a><br> FAX: 508-495-2258 </i></p> <p> <i> Updated November 15, 2005; gfh </i> </pre> The 1995 and 1996 bottle data were collected with a GO rosette mounted above the MK5 CTD. The temperature, conductivity, salinity, and fluorescence data were collected from the CTD data stream when the bottle was tripped (~30 scans are averaged). 10010 ctd_cg ctd_cg http://globec.whoi.edu/jg/serv/globec/gb/ctd_cg.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/ctd_cg%7D <h2 align=center>CTD Hydrography</h2> <h2 align=center> Endeavor 307, 330, 331 and Oceanus 332, 334</h2> <p> <p> click <a href="http://globec.whoi.edu/jg/info/globec/gb/ctd_cg_notes">here</a> for additional sampling information (SeaBird System output). <p> Questions regarding these data should be directed to the US GLOBEC <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a>. <p> <b>DMO Notes:</b><br> The data reported here are from the primary CTD sensors. However, this data set also contains conductivity, temperature and related computed parameters from secondary sensors. If these data are of interest, please contact the Data Management Office at the above link.<br> </p><p> * Temperatures are reported in ITS90 scale except for Endeavor cruise 307 which are in the ITS68 scale. </p> <pre> <b>Chief Scientist:</b> Charles Greene Cornell University <b>Contributor:</b> Heidi Sosik Woods Hole Oceanographic Institution</td></tr> <i> prepared by: Dicky Allison, March 2003 updated: October 1, 2004; gfh </i></pre> The data reported here are from the primary CTD sensors. However, this data set also contains conductivity, temperature and related computed parameters from secondary sensors. <pre> <b>Header details:</b> # pr = pressure [db] # t090 = temperature, pri, ITS-90 [deg C] # c0S/m = conductivity, primary [S/m] # t190 = temperature, sec, ITS-90 [deg C] # c1S/m = conductivity, secondary [S/m] # flS = fluorometer, sea tech # xmiss = transmissometer # sal00 = salinity, PSS-78 [PSU], T0, C0 # sal11 = salinity, PSS-78 [PSU], T1, C1 # potemp068 = potential temperature, pri, IPTS-68 [deg C] # potemp090 = potential temperature, pri, ITS-90 [deg C] # depS = depth, salt water [m] # density00 = density [kg/m^3], T0, C0 # sigma-È00 = density, sigma-theta [kg/m^3], T0, C0 # sigma-t00 = density, sigma-t [kg/m^3], T0, C0 # sigma-100 = density, sigma-1 [kg/m^3], T0, C0 # sigma-200 = density, sigma-2 [kg/m^3], T0, C0 # sigma-400 = density, sigma-4 [kg/m^3], T0, C0 # oxsatML/L = oxygen saturation [ml/l] # nbin = number of scans per bin # interval = decibars: 1 # bad_flag = -9.990e-29 # sensor 0 = Frequency 0 temperature, primary, 2107, 03 FEB-99 # sensor 1 = Frequency 1 conductivity, primary, 1745, 05-FEB-99s, cpcor = -9.5700e-08 # sensor 2 = Frequency 2 pressure, 64853, 08-21-96 # sensor 3 = Frequency 3 temperature, secondary, 2034, 03-FEB-99s # sensor 4 = Frequency 4 conductivity, secondary, 1749, 03-FEB-99s, cpcor = -9.5700e-08 # sensor 5 = Extrnl Volt 0 transmissometer, 243D, 10 Jul 1999 # sensor 6 = Extrnl Volt 1 fluorometer, sea tech, 30s, july 1987 # sensor 7 = Extrnl Volt 2 oxygen, current, 130454, 18 AUG 1999 # sensor 8 = Extrnl Volt 3 oxygen, temperature, 130454, 18 AUG 1999 # sensor 9 = Extrnl Volt 4 irradiance (PAR), 4479, AUG 15, 1996 # sensor 10 = Extrnl Volt 9 surface irradiance (SPAR), degrees = 0.0 </pre> 10011 ctd_dg ctd_dg http://globec.whoi.edu/jg/serv/globec/gb/ctd_dg.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/ctd_dg%7D <h2 align=center>CTD Hydrography, Endeavor 321 and 325</h2> <p> <p>Click <a href="http://globec.whoi.edu/jg/info/globec/gb/ctd_dg_notes">here</a> for additional sampling information (SeaBird system output). <p> Questions regarding these data should be directed to the US GLOBEC <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a>. <p> <b>DMO Note:</b><br> The data reported here are from the primary CTD sensors. However, this data set also contains conductivity, temperature and related computed parameters from secondary sensors. If these data are of interest, please contact the Data Management Office at the above link. </p> <pre> <b>Chief Scientist:</b> Dian Gifford University of Rhode Island Graduate School of Oceanography <i>prepared by: Dicky Allison, March 2003 updated: gfh, 4 October 2004 </i> </pre> The data reported here are from the primary CTD sensors. However, this data set also contains conductivity, temperature and related computed parameters from secondary sensors. <pre> <b>Header Details:</b> # nquan = 14 # nvalues = 75 # units = metric # pr = pressure [db] # c0S/m = conductivity, primary [S/m] # c1S/m = conductivity, secondary [S/m] # t090 = temperature, pri, ITS-90 [deg C] # t190 = temperature, sec, ITS-90 [deg C] # xmiss = transmissometer # flS = fluorometer, sea tech # oxML/L = oxygen [ml/l] # par = irradiance (PAR) # nbf = number of bottles fired # sal00 = salinity, PSS-78 [PSU], T0, C0 # sal11 = salinity, PSS-78 [PSU], T1, C1 # sigma-t00 = density, sigma-t [kg/m^3], T0, C0 # nbin = number of scans per bin # interval = decibars = 1 # start_time = Mar 31 1999 13:48:50 # bad_flag = -9.990e-29 # sensor 0 = Frequency 0 temperature, primary, 2107, 03 FEB-99 # sensor 1 = Frequency 1 conductivity, primary, 1745, 05-FEB-99s, cpcor = -9.5700e-08 # sensor 2 = Frequency 2 pressure, 64853, 08-21-96 # sensor 3 = Frequency 3 temperature, secondary, 2034, 03-FEB-99s # sensor 4 = Frequency 4 conductivity, secondary, 1749, 03-FEB-99s, cpcor = -9.5700e-08 # sensor 5 = Extrnl Volt 0 transmissometer, 243D, 16 FEB 1999 # sensor 6 = Extrnl Volt 1 fluorometer, sea tech, 30s, july 1987 # sensor 7 = Extrnl Volt 2 oxygen, current, 130454, 18 AUG 1999 # sensor 8 = Extrnl Volt 3 oxygen, temperature, 130454, 18 AUG 1999 # sensor 9 = Extrnl Volt 4 irradiance (PAR), 4479, AUG 15, 1996 # sensor 10 = Extrnl Volt 9 surface irradiance (SPAR), degrees = 0.0 </pre> 10012 ctd_mocness10 ctd_mocness10 http://globec.whoi.edu/jg/serv/globec/gb/ctd_mocness.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/ctd_mocness%7D <p> The MOCNESS is based on the Tucker Trawl principle (Tucker, 1951). The particular MOCNESS system from which these CTD data came is one of three net systems. The MOCNESS-10 (with 10 m² nets)carries 6 nets of 3.0-mm circular mesh which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976). In all three systems, "the underwater unit sends a data frame, comprised of temperature, depth, conductivity, net-frame angle, flow count, time, number of open net, and net opening/closing, to the deck unit in a compressed hexadecimal format every 2 seconds and from the deck unit to a microcomputer every 4 seconds... Temperature (to approximately 0.01 deg C) and conductivity are measured with SEABIRD sensors. Normally, a modified T.S.K.-flowmeter is used... Both the temperature and conductivity sensors and the flowmeter are mounted on top of the frame so that they face horizontally when the frame is at a towing angle of 45deg... Calculations of salinity (to approximately 0.01 o/oo S), potential temperature (theta), potential density (sigma), the oblique and vertical velocities of the net, and the approximate volume filtered by each net are made after each string of data has been received by the computer." (Wiebe <i>et al.</i>, 1985) In addition, data were collected from four other sensors attached to the frame: the Transmissometer, the Fluorometer, the Downwelling light sensor, and the Oxygen sensor. A SeaBird underwater pump was also included in the sensor suite. </p> <p><b> It should be noted that whenever the data are of questionable value, "50.000" is written in the particular data field. </b> </p> <p><u>The following notes are cruise-specific:</u><br> <b>OC319:</b> Lats and Lons for first two tows are missing because gps string not yet available.</p> <p>Unless otherwise indicated, these data have not been post-processed.</p> <p>For additional information, contact the <a href="http://usjgofs.whoi.edu/jg/serv/globec/gb/inventory.html0?project,name_prin"> chief scientist</a> for the cruise or the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">U.S. GLOBEC Data Management Office</a> (DMO). </p> <p> <b>Note:</b> Some variables have been eliminated from the display but are nevertheless available. These variables include: oxycurrent, oxytemp, tempco, and echo.</p> <pre> <h2>References</h2> Fofonoff and Millard, 1983, UNESCO technical papers in Marine Sciences, #44 Tucker, G.H., 1951. Relation of fishes and other organisms to the scattering of underwater sound. <i> Journal of Marine Research</i>, <b>10:</b> 215-238. Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. <i>Journal of Marine Research</i>, <b>34(3):</b> 313-326 Wiebe, P.H., A.W. Morton, A.M. Bradley, R.H. Backus, J.E. Craddock, V. Barber, T.J. Cowles and G.R. Flierl, 1985. New developments in the MOCNESS, an apparatus for sampling zooplankton and micronekton. <i>Marine Biology</i>, <b>87:</b> 313-323. <i> updated October 27 2005, gfh</i> </pre> The underwater unit sends a data frame, comprised of temperature, depth, conductivity, net-frame angle, flow count, time, number of open net, and net opening/closing, to the deck unit in a compressed hexadecimal format every 2 seconds and from the deck unit to a microcomputer every 4 seconds... Temperature (to approximately 0.01 deg C) and conductivity are measured with SEABIRD sensors. Normally, a modified T.S.K.-flowmeter is used... Both the temperature and conductivity sensors and the flowmeter are mounted on top of the frame so that they face horizontally when the frame is at a towing angle of 45deg... Calculations of salinity (to approximately 0.01 o/oo S), potential temperature (theta), potential density (sigma), the oblique and vertical velocities of the net, and the approximate volume filtered by each net are made after each string of data has been received by the computer. 10013 ctd_rl ctd_rl http://globec.whoi.edu/jg/serv/globec/gb/ctd_rl.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/ctd_rl%7D <h2 align=center>Process Study CTD data, Gulf of Maine/Georges Bank</h2> <p> <b>Contributor:</b><br> Richard Limeburner<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br> <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a><br><br> <b>Dataset:</b><br> Process Study CTD data, Gulf of Maine/Georges Bank<br> <p> <b>NOTE:</b><br> These data sets should be considered preliminary. A cursory quality review has been performed and the results of this review are tabulated below on a cruise by cruise basis.<br></p> <p> <p> <b>CHARLES ISELIN CRUISE 9407, CTD DATA QUALITY REVIEW</b><br> <p> GENERAL COMMENT: THIS DATA SET IS OF POOR QUALITY, USE "CAUTION".<br> <P> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CASTS 96 AND 98 CONTAIN ONLY A SURFACE DATA CYCLE. FILES DELETED. 3..OXYGEN BAD ALL CASTS. REPLACED WITH -9..<br> 4..SALINITY IS NOISY. SOME CASTS WORSE THEN OTHERS. NO ATTEMPT TO CLEAN UP. USE WITH CAUTION.<br> 5..LIGHT TRANSMISSION. CASTS 68 - 99 SHOW A ONE VOLT OFFSET FROM CASTS 1-68. CALIBARATION PROBLEM? USE WITH CAUTION. NO ATTEMPT TO CLEAN UP SPIKES.<br> 6..FLUORESCENCE. CASTS 68 - 99 SHOW A TWO VOLT OFFSET FROM CASTS 1 - 68. CALIBRATION PROBLEM? USE WITH CAUTION. NO ATTEMPT TO CLEAN UP SPIKES.<br></p> <p> <b>ENDEAVOR CRUISE 259, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION WAS EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..NO CTD CAST 20. APPEARS TO BE THE RESULT OF MIS-NUMBERING.<br> 3..CTD CAST 13 HAS ONLY ONE DATA CYCLE, SURFACE VALUE. FILE DELETED.<br> 4..CTD CAST 27. THE DATA REPORTED FOR CAST 27 IS THE EXACT SAME AS FOR CAST 28. THE FILE FOR CAST 27 DELETED.<br> 5..CTD CAST 29. FLUOROMETER DATA BAD ENTIRE CAST, REPLACED WITH -9.0 BAD/MISSING DATA INDICATOR.<br> 6..CTD CAST 30. TRANSMISSOMETER DATA, DATA SPIKE AT 274 DECIBARS. REPLACED WITH -9.0.<br> 7..OXYGEN DISPLAYS OCCASIONAL DATA SPIKES AND SHIFTS EXTENDING OVER MORE THEN ONE DECIBAR. NO ACTION TAKEN<br></p> <p> <b>ENDEAVOR CRUISE 260, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION WAS EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CAST NUMBERS 26, 27 AND 28 MISSING.<br> 3..OXYGEN DISPLAYS OCCASIONAL DATA SPIKES EXTENDING OVER MORE THEN ONE DECIBAR (CAST 13 AT 110 DECIBARS, AND CAST 16 AT 41 DECIBARS). NO ACTION TAKEN.<br></p> <p> <b>ENDEAVOR CRUISE 262, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CAST NUMBERS 20, AND 21. ALL OXYGEN VALUES BAD. REPLACED WITH -9..<br> 3..LIGHT TRANSMISSION. ONE DECIBAR DATA SPIKES REMOVED FROM CAST 2, 5 AND 23, SURFACE VALUES. A ONE DECIBAR SPIKE REMOVED FROM CAST 21 AT 14 DECIBARS.<br> 4..FLUORESCENCE. DATA SPIKE REMOVED FROM CAST 21 AT 14 DECIBARS.<br></p> <p> <b>ENDEAVOR CRUISE 264, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CAST NUMBERS 29, 30, 32, AND 34 MISSING.<br> 3..LIGHT TRANSMISSION. ONE DECIBAR DATA SPIKES REMOVED FROM CAST 2 AT 10M, AND CAST 23 AT 88M.<br></p> <p> <b>ENDEAVOR CRUISE 266, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..DATA FOR CAST NUMBERS 22, AND 23 MISSING.<br></p> <p> <b>ENDEAVOR CRUISE 267 LEG 1, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..DATA FOR CAST NUMBERS 4, 98, AND 103 MISSING.<br> 3..CAST 1 AND 81 ALL VALUES REMOVED FROM LAST DATA CYCLE DUE TO DATA SPIKES.<br> 4..FLUORESCENCE. DATA OFF SCALE ON THE HIGH SIDE. SEVERAL CASTS EXCEED THE MAX. OF VALUE OF 5 VOLTS.<br></p> <p> <b>ENDEAVOR CRUISE 267 LEG 2, CTD DATA QUALITY REVIEW</b><br> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..ONE DECIBAR SALINITY SPIKES REMOVED FROM STATION 210 at 24m, 214 at 16m and 217 at 4m.<br></p> <p> <b>ENDEAVOR CRUISE 269, CTD DATA QUALITY REVIEW</b> <p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CAST 30, FLUORESCENCE DATA SPIKE AT 69 METERS REMOVED.<br> 3..OXYGEN VERY NOISY (LARGE NUMBER OF SPIKES). NO ACTION TAKEN. USE WITH CAUTION.<br></p> <p> <i> updated: November 16, 2005; gfh </i></p> Process Study CTD data, Gulf of Maine/Georges Bank. <b>CHARLES ISELIN CRUISE 9407, CTD DATA QUALITY REVIEW</b><br> </p><p> GENERAL COMMENT: THIS DATA SET IS OF POOR QUALITY, USE "CAUTION".<br> </p><p> 1..CAST SAMPLING INFORMATION EDITED TO BE CONSISTENT WITH THE EVENT LOG. DATES AND TIMES ARE REPORTED AS GMT.<br> 2..CASTS 96 AND 98 CONTAIN ONLY A SURFACE DATA CYCLE. FILES DELETED. 3..OXYGEN BAD ALL CASTS. REPLACED WITH -9..<br> 4..SALINITY IS NOISY. SOME CASTS WORSE THEN OTHERS. NO ATTEMPT TO CLEAN UP. USE WITH CAUTION.<br> 5..LIGHT TRANSMISSION. CASTS 68 - 99 SHOW A ONE VOLT OFFSET FROM CASTS 1-68. CALIBARATION PROBLEM? USE WITH CAUTION. NO ATTEMPT TO CLEAN UP SPIKES.<br> 6..FLUORESCENCE. CASTS 68 - 99 SHOW A TWO VOLT OFFSET FROM CASTS 1 - 68. CALIBRATION PROBLEM? USE WITH CAUTION. NO ATTEMPT TO CLEAN UP SPIKES.<br></p> 10014 drifter_images drifter_images http://globec.whoi.edu/jg/serv/globec/gb/drifters.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter_images%7D <pre> <b>PI:</b> R.Limeburner <b>dataset:</b> Drifter tracks <p>Note, for the "flc" animations you will need a movie player capable of reading *.fli/*.flc type movies. The <a href="http://usjgofs.whoi.edu/globec-dir/aaplay.html">Autodesk Animation Player</a> is one such player. </pre> 10015 drifter_positions drifter_positions http://globec.whoi.edu/jg/serv/globec/gb/drifter_positions.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter_positions%7D <h2 align=center>Initial Drifter Deployment Positions, 1998, Georges Bank</h2> <p> <b>DMO Notes:</b><br> ¹Drifters named with a leading "g" were generally deployed in US terriorial waters and drifters identified with a leading "n" were deployed in Canadian Waters by Peter Smith from the Bedford Institute of Oceanography (BIO). Also Drifter types containing a gps system reported positions every 30 minutes.<br></p> ²Type parameter is a combination of:<br> Manufacture code, se = Seimac, cw = Clearwater, met = MEtocean, to = Technocean<br> Center depth of drogue, 10 or 40 meters<br> Shape of drogue, W = wide verses a square drogue<br> Presence of gps system = gps<br> <pre> <b>Contributor:</b> Richard Limeburner Woods Hole Oceanographic Institution Woods Hole, MA 02540 <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a> <i>updated: December 09, 2004; GHeimerdinger</i> </pre> 10016 drifter95 drifter95 http://globec.whoi.edu/jg/serv/globec/gb/drifter95.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter95%7D <h2 align=center>Raw drifter data (1995)</h2> <p> <b>DMO Notes:</b><br> ¹All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year).<br></p> Based on dates of deployment and recovery, a drifter file may span two calendar years. <p> ²The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled.<br><br> <b>REF:</b><br> Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 <br> reports on the 1995-1997 deployments: </p> <pre> <b>Contributor:</b> Richard Limeburner Woods Hole Oceanographic Institution Woods Hole, MA 02540 <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a> <i>updated: Aug 26, 2005; gfh</i> </pre></pre> Raw drifter data (1995) 1All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. 10017 drifter96 drifter96 http://globec.whoi.edu/jg/serv/globec/gb/drifter96.html0%7Bdir=globec.whoi.edu/jg/dir/glob ec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter96%7D <h2 align=center>Raw drifter data (1996)</h2> <p> <b>DMO Notes:</b><br> ¹All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year).<br></p> Based on dates of deployment and recovery, a drifter file may span two calendar years. <p> ²The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled.<br><br> <b>REF:</b><br> Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 <br> reports on the 1995-1997 deployments: </p> <pre> <b>Contributor:</b> Richard Limeburner Woods Hole Oceanographic Institution Woods Hole, MA 02540 <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a> <i>updated: Aug 26, 2005; gfh</i> </pre> </pre> Raw drifter data (1996) All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. REF: Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 reports on the 1995-1997 deployments. 10018 drifter97 drifter97 http://globec.whoi.edu/jg/serv/globec/gb/drifter97.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter97%7D <h2 align=center>Raw drifter data (1997)</h2> <p> <b>DMO Notes:</b><br> ¹All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year).<br></p> Based on dates of deployment and recovery, a drifter file may span two calendar years. <p> ²The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled.<br><br> <b>REF:</b><br> Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 <br> reports on the 1995-1997 deployments: </p> Raw drifter data (1997) DMO Notes: 1All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. 10019 drifter98 drifter98 http://globec.whoi.edu/jg/serv/globec/gb/drifter98.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter98%7D <h2 align=center>Raw drifter data (1998)</h2> <p> <b>DMO Notes:</b><br> ¹All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year).<br></p> Based on dates of deployment and recovery, a drifter file may span two calendar years. <p> ²The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled.<br><br> <b>REF:</b><br> Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 <br> reports on the 1995-1997 deployments: </p> <pre> <b>Contributor:</b> Richard Limeburner Woods Hole Oceanographic Institution Woods Hole, MA 02540 <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a> <i>updated: Aug 26, 2005; gfh</i> </pre> </pre> Drifter data (1998) 1All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. 10020 drifter99 drifter99 http://globec.whoi.edu/jg/serv/globec/gb/drifter99.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/drifter99%7D <h2 align=center>Raw drifter data (1999)</h2> <p> <b>DMO Notes:</b><br> ¹All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year).<br></p> Based on dates of deployment and recovery, a drifter file may span two calendar years. <p> ²The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled.<br><br> ³Those drifters with identifications starting with a "g" were generally deployed in US territorial waters and those with an "n" deployed in Canadian waters by the Bedford Institute of Oceanography.<br><br> <b>REF:</b><br> Christopher E. Naimie, Richard Limeburner, Charles G. Hannah and Robert C. Beardsley, 2001. On the geographic and seasonal patterns of the near-surface circulation on Georges Bank - from real and simulated drifters. Deep-Sea Research II 48, Pages 501-518 <br> reports on the 1995-1997 deployments: </p> <pre> <b>Contributor:</b> Richard Limeburner Woods Hole Oceanographic Institution Woods Hole, MA 02540 <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a> <i>updated: Aug 26, 2005; gfh</i> </pre> </pre> Raw drifter data (1999) 1All drifters submitted by this investigator, regardless of year deployed, have a year day (yrday) value beginning with January 1, 1995 (year day of 1.0000). Thus a deployment in 1996 will have a year day >365.0000 and a deployment in 1999 will have a deployment year day value >1461.0000 (1998 a leap year). Based on dates of deployment and recovery, a drifter file may span two calendar years. 2The status of drogue presence is indicated by timing the submergence of the surface float. When the drogue is attached its drag will cause the surface sphere to submerge occasionally as a wave passes. If the drogue has been lost, the surface sphere remains at the surface and is not buried by waves. When the surface float submerges, contacts on top of the sphere are shorted out by the seawater and the PTT controller starts counting the length of time (seconds) the contacts are shorted. Every 30 minutes the accumulated submergence time is scaled by 0.1 (for example, 1000 seconds is scaled to 100) and loaded into the first byte of the data string and a new submergence time is started. Typical submergence values are 10 to 100. Consistent submergence values of 0, indicate the drogue has been lost. The maximum submergence value is 180 and indicates the surface float is sinking, or heavily fouled. 3Those drifters with identifications starting with a "g" were generally deployed in US territorial waters and those with an "n" deployed in Canadian waters by the Bedford Institute of Oceanography. 10021 emet_W60_1995 emet_W60_1995 http://globec.whoi.edu/jg/serv/globec/gb/emet_W60_1995.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W60_1995%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 60 minute averaged values, 1995</h2> <p> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, Ma 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li> Concatenate daily 1 minute files into one file for whole cruise <li> Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li> Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li> Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li> Iterate steps 2-4 until no more obvious bad points. <li> Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li> Check plots of true wind speed and direction to make sure they look ok. <li> Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </ol> <pre> Edo depth error correction: replace bad value with previous value. EN268 - Data gap 20:47:17 to 24:00:00 on last day. Filled it with linearly interpolated data. There was a problem with short wave formatting in raw data. Values > 999.9 read ****. Replaced garbage with 999.9 except for a few not near the middle of the day which were replaced with previous value. A number of gaps in Edo depth. 8465 records, 284 interpolated. Cruise Exp Spds Dirs AT RH BP SST EDOZ LWR SWR Comments EN268 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10022 emet_W15_1995 emet_W15_1995 http://globec.whoi.edu/jg/serv/globec/gb/emet_W15_1995.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W15_1995%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 15 minute averaged values, 1995</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, Ma 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise </li><li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. </li><li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 &amp; 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m &amp; 1m depth, Edo depth, Chirp sonar depth. </li><li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. </li><li>Iterate steps 2-4 until no more obvious bad points. </li><li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. </li><li>Check plots of true wind speed and direction to make sure they look ok. </li><li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m &amp; 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN268 - Data gap 20:47:17 to 24:00:00 on last day. Filled it with linearly interpolated data. There was a problem with short wave formatting in raw data. Values > 999.9 read ****. Replaced garbage with 999.9 except for a few not near the middle of the day which were replaced with previous value. A number of gaps in Edo depth. 8465 records, 284 interpolated. Cruise Exp Spds Dirs AT RH BP SST EDOZ LWR SWR Comments EN268 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10023 emet_W1_1995 emet_W1_1995 http://globec.whoi.edu/jg/serv/globec/gb/emet_W1_1995.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W1_1995%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 1 minute values, 1995</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, Ma 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 28, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise </li><li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. </li><li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 &amp; 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m &amp; 1m depth, Edo depth, Chirp sonar depth. </li><li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. </li><li>Iterate steps 2-4 until no more obvious bad points. </li><li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. </li><li>Check plots of true wind speed and direction to make sure they look ok. </li><li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m &amp; 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN268 - Data gap 20:47:17 to 24:00:00 on last day. Filled it with linearly interpolated data. There was a problem with short wave formatting in raw data. Values > 999.9 read ****. Replaced garbage with 999.9 except for a few not near the middle of the day which were replaced with previous value. A number of gaps in Edo depth. 8465 records, 284 interpolated. Cruise Exp Spds Dirs AT RH BP SST EDOZ LWR SWR Comments EN268 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10024 emet_W60_1996 emet_W60_1996 http://globec.whoi.edu/jg/serv/globec/gb/emet_W60_1996.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W60_1996%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 60 minute averaged values, 1996</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, Ma 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN276 - Data gap from 20:11:57 Jan 19 (19.84163) through 18:21:52 Jan 20 (20.76519). Linearly interpolated through it except for SW. Linear interpolation of SW from 19.84163 to zero at sunset, -4.0 until sunrise, linear interpolation to value at 20.76588. Edo depth had a lot of error values which were mostly correctible. 18,110 records, 1330 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN276 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10025 emet_W15_1996 emet_W15_1996 http://globec.whoi.edu/jg/serv/globec/gb/emet_W15_1996.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W15_1996%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 15 minute averaged values, 1996</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, Ma 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> Additional <a href="http://usjgofs.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. <p> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN276 - Data gap from 20:11:57 Jan 19 (19.84163) through 18:21:52 Jan 20 (20.76519). Linearly interpolated through it except for SW. Linear interpolation of SW from 19.84163 to zero at sunset, -4.0 until sunrise, linear interpolation to value at 20.76588. Edo depth had a lot of error values which were mostly correctible. 18,110 records, 1330 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN276 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10026 emet_W1_1996 emet_W1_1996 http://globec.whoi.edu/jg/serv/globec/gb/emet_W1_1996.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W1_1996%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 1 minute values, 1996</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 28, 2004; G.Heimerdinger </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN276 - Data gap from 20:11:57 Jan 19 (19.84163) through 18:21:52 Jan 20 (20.76519). Linearly interpolated through it except for SW. Linear interpolation of SW from 19.84163 to zero at sunset, -4.0 until sunrise, linear interpolation to value at 20.76588. Edo depth had a lot of error values which were mostly correctible. 18,110 records, 1330 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN276 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10027 emet_W60_1997 emet_W60_1997 http://globec.whoi.edu/jg/serv/globec/gb/emet_W60_1997.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W60_1997%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 60 minute averaged values, 1997</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> The data quality is generally pretty poor on the Oceanus cruises. OC297 and OC298 have no SOG, COG, or gyro so I could not correct the winds. I almost set the TWS, TWD to 0 but decided to leave them in as RWS, RWD. One could get a semiqualitative feel for the winds. OC301 had gyro but no SOG, COG so I computed them from the GPS position differences. It came out better than I expected. Warn users to be skeptical about the Oceanus data. <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN296 - Second GPS missing through most of file. Not significant since I usually use the Trimble. About 2 hours of SW & LW data missing on day 69 in early afternoon. Heavy clouds so SW low and LW steady. Interpolated values. Only a very few Edo depth values. 18067 records, 8 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN296 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10028 emet_W15_1997 emet_W15_1997 http://globec.whoi.edu/jg/serv/globec/gb/emet_W15_1997.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W15_1997%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 15 minute averaged values, 1997</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> The data quality is generally pretty poor on the Oceanus cruises. OC297 and OC298 have no SOG, COG, or gyro so I could not correct the winds. I almost set the TWS, TWD to 0 but decided to leave them in as RWS, RWD. One could get a semiqualitative feel for the winds. OC301 had gyro but no SOG, COG so I computed them from the GPS position differences. It came out better than I expected. Warn users to be skeptical about the Oceanus data. <p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN296 - Second GPS missing through most of file. Not significant since I usually use the Trimble. About 2 hours of SW & LW data missing on day 69 in early afternoon. Heavy clouds so SW low and LW steady. Interpolated values. Only a very few Edo depth values. 18067 records, 8 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN296 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10029 emet_W1_1997 emet_W1_1997 http://globec.whoi.edu/jg/serv/globec/gb/emet_W1_1997.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W1_1997%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 1 minute values, 1997</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> Specific notes: <p> The data quality is generally pretty poor on the Oceanus cruises. OC297 and OC298 have no SOG, COG,or gyro so I could not correct the winds. I almost set the TWS, TWD to 0 but decided to leave them in as RWS, RWD. One could get a semiqualitative feel for the winds. OC301 had gyro but no SOG, COG so I computed them from the GPS position differences. It came out better than I expected. Warn users to be skeptical about the Oceanus data. </p> <i>From: Richard E. Payne / 11 Apr 1997 09:05:25 -0400<br> Updated: April 28, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN296 - Second GPS missing through most of file. Not significant since I usually use the Trimble. About 2 hours of SW & LW data missing on day 69 in early afternoon. Heavy clouds so SW low and LW steady. Interpolated values. Only a very few Edo depth values. 18067 records, 8 interpolated. Cruise Exp Spds Dirs AT RH BP SST SSC SWR Prec EN296 GLOBEC --- --- --- --- --- --- --- --- --- </pre> 10030 emet_W60_1998 emet_W60_1998 http://globec.whoi.edu/jg/serv/globec/gb/emet_W60_1998.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W6 0_1998%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 60 minute averaged values, 1998</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre><p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. </p><h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise </li><li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. </li><li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. </li><li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. </li><li>Iterate steps 2-4 until no more obvious bad points. </li><li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. </li><li>Check plots of true wind speed and direction to make sure they look ok. </li><li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne, April 27, 1998<br> Updated: April 29, 2004; G.Heimerdinger </i> </p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li> Concatenate daily 1 minute files into one file for whole cruise <li> Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li> Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li> Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li> Iterate steps 2-4 until no more obvious bad points. <li> Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li> Check plots of true wind speed and direction to make sure they look ok. <li> Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </ol> <pre> Edo depth error correction: replace bad value with previous value. OC333 - Raw water depth included for first time but data were useless. Cruise Exp Spds Dirs AT RH BP SST SWR Prec SSC SSAL OC333 GLOBEC Good Good Good Good Good Good Good Good Noisy VNoisy </pre> 10031 emet_W15_1998 emet_W15_1998 http://globec.whoi.edu/jg/serv/globec/gb/emet_W15_1998.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W15_1998%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 15 minute averaged values, 1998</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne, April 27, 1998<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. OC333 - Raw water depth included for first time but data were useless. Cruise Exp Spds Dirs AT RH BP SST SWR Prec SSC SSAL OC333 GLOBEC Good Good Good Good Good Good Good Good Noisy VNoisy </pre> 10032 emet_W1_1998 emet_W1_1998 http://globec.whoi.edu/jg/serv/globec/gb/emet_W1_1998.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W1_1998%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 1 minute values, 1998</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne, April 27, 1998<br> Updated: April 28, 2004; G.Heimerdinger </i></pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. OC333 - Raw water depth included for first time but data were useless. Cruise Exp Spds Dirs AT RH BP SST SWR Prec SSC SSAL OC333 GLOBEC Good Good Good Good Good Good Good Good Noisy VNoisy </pre> 10033 emet_W60_1999 emet_W60_1999 http://globec.whoi.edu/jg/serv/globec/gb/emet_W60_1999.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W60_1999%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 60 minute averaged values, 1999</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne October 25, 1999<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN323 - Good data. Air temp noisy. The noise has been traced to stack gases passing over the RH and AT sensors as the ship turns. This causes the AT to be momentarily anomalously high and the RH low. Edo depth not useful. EN323 GLOBEC --- --- --- --- --- --- --- --- --- --- </pre> 10034 emet_W15_1999 emet_W15_1999 http://globec.whoi.edu/jg/serv/globec/gb/emet_W15_1999.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W15_1999%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 15 minute averaged values, 1999</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne, May 28, 1999<br> Updated: April 29, 2004; G.Heimerdinger </i> </pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN323 - Good data. Air temp noisy. The noise has been traced to stack gases passing over the RH and AT sensors as the ship turns. This causes the AT to be momentarily anomalously high and the RH low. Edo depth not useful. EN323 GLOBEC --- --- --- --- --- --- --- --- --- --- </pre> 10035 emet_W1_1999 emet_W1_1999 http://globec.whoi.edu/jg/serv/globec/gb/emet_W1_1999.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/emet_W1_1999%7D <h2 align=center>Continuous along track meteorology and sea surface data,<br> 1 minute values, 1999</h2> <pre> <b>Processed by:</b> Richard Payne Woods Hole Oceanographic Institution Woods Hole, MA 20543 <a href="mailto:rpayne@whoi.edu">rpayne@whoi.edu</a> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/additional_endeavor_processing_details.html">data processing notes</a> are available. </pre> <p> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <h3>Processing Notes</h3> <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <p> <i>From: Richard E. Payne May 28, 1999<br> Updated: April 28, 2004; G.Heimerdinger </i></pre> The sea surface temperature as measured by the hull sensor is not shown since the sea surface temperature as measured via the engine inlet (field name is temp_ss1) is more accurate. <ol> <li>Concatenate daily 1 minute files into one file for whole cruise <li>Edit file for obvious bad data, i.e., missing data, garbage characters, etc. <li>Run program which reformats data. Output parameters:<br> Year day, lat, long, Speed made good, course made good, gyro 1 & 2, Edo speed, Edo indicator, port wind speed, starboard ws, port wind azimuth, starboard waz, air temp, relative humidity, barometric pressure, sea surface temp @5m & 1m depth, Edo depth, Chirp sonar depth. <li>Put plots of all parameters on screen and look for obvious single bad points. Edit in basic concatenated file. Except I have not edited depths. <li>Iterate steps 2-4 until no more obvious bad points. <li>Run second program which computes true wind speed and direction from speed and course made good, gyros, larger of port or starboard ws and accompanying wind azimuth. Outputs are year day, lat lon, speed and course made good, gyro, relative ws and direction, true ws and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation,5m and 1m sea surface temps, Edo depth, Chirp sonar depth, Edo speed, Edo indicator. <li>Check plots of true wind speed and direction to make sure they look ok. <li>Run vector averaging program which produces 60 minute series. The program uses 60 consecutive records and does not check for missing records. I have not carried depths since hourly averages do not seem useful nor Edo speeds since they seem pretty generally useless. Output parameters are: Year day, lat, long, true wind speed and direction, air temp, relative humidity, barometric pressure, short- and long-wave radiation, sea surface temp @ 5m & 1m. </li></ol> <pre> Edo depth error correction: replace bad value with previous value. EN323 - Good data. Air temp noisy. The noise has been traced to stack gases passing over the RH and AT sensors as the ship turns. This causes the AT to be momentarily anomalously high and the RH low. Edo depth not useful. EN323 GLOBEC --- --- --- --- --- --- --- --- --- --- </pre> 10036 eventlogs eventlogs http://globec.whoi.edu/jg/serv/globec/gb/eventlogs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/eventlogs%7D <p> Event logs provide an overall summary of the sampling activities during a cruise. A hard copy of the event log is also included in the <a href="http://globec.whoi.edu/globec-dir/cruise-reports.html">cruise report</a>. Further documentation about event logs is available in <a href="http://globec.whoi.edu/globec-dir/require.html">Chief Scientist Data Reporting Requirements</a>. </p> <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a></p> <i>Last updated November 03, 2006; gfh</i> Cruise Event Log Event logs provide an overall summary of the sampling activities during a cruise. A hard copy of the event log is also included in the cruise report. Further documentation about event logs is available in Chief Scientist Data Reporting Requirements. 10037 fisheggs fisheggs http://globec.whoi.edu/jg/serv/globec/gb/fisheggs_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/fisheggs%7D <h3 align=center>Georges Bank Fish Egg Data from Bongo Nets</h3> <p> ¹Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m² of sea surface area. Most haul factors range from 1 to 10. The Standard Haul Factor has not been applied to the data reported here. </p> <p> ²Stages 6, 7, 8, & 9 are used only for Gadidae eggs. </p> <pre> <b>Any questions, contact:</b> John Sibunka National Marine Fisheries Service, NEFC Sandy Hook Marine Lab. 74 Magruder Road Highlands, NJ 07732 voice: (732) 872-3064 fax: (732) 872-3088 <a href="mailto:John.Sibunka@noaa.gov">John.Sibunka@noaa.gov</a> <i>updated July 8, 2005, G.Heimerdinger </i> </pre> Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m2 of sea surface area. Most haul factors range from 1 to 10. The Standard Haul Factor has not been applied to the data reported here. 10038 fishlarvaeB fishlarvaeB http://globec.whoi.edu/jg/serv/globec/gb/fishlarvaeB_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/fishlarvaeB%7D <h2 align=center>Georges Bank Fish Larvae Data from Bongo Nets</h2> <p> ¹Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m2 of sea surface area. Most haul factors range from 1 to 10. The Standard Haul Factor has not been applied to the data reported here.<br> <br> Specifics on bongo tow displacement volumes can be seen on the companion file "bongovols" under the heading of broadscale cruises. </p> <pre> <b>Any questions, contact:</b> Donna Johnson National Marine Fisheries Service Sandy Hook Laboratory 74 Magruder Road Highlands, NJ 07732 voice: (732) 872-3092 fax: (732) 872-3088 email: <a href="mailto:djohnson@snook.sh.nmfs.gov">djohnson@snook.sh.nmfs.gov</a> <i>updated: June 3, 2004, G.Heimerdinger </i> </pre> GLOBEC Fish Larvae collected by Bongo nets,Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m2 of sea surface area. Most haul factors range from 1 to 10. The Standard Haul Factor has not been applied to the data reported here. 10039 fishlarvaeM fishlarvaeM http://globec.whoi.edu/jg/serv/globec/gb/fishlarvaeM_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/fishlarvaeM%7D <h2 align=center>Georges Bank Fish Larvae Data from MOCNESS tows</h2> <p> ¹Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m2 of sea surface area. Most haul factors range from 1 to 10. The Standard Haul Factor has not been applied to the data reported here. </p> <pre><b>Any questions, contact:</b> Donna Johnson National Marine Fisheries Service, NEFC Sandy Hook Laboratory 74 Magruder Road Highlands, NJ 07732 voice: (732) 872-3092 fax: (732) 872-3088 e-mail: <a href="mailto:djohnson@snook.sh.nmfs.gov">djohnson@snook.sh.nmfs.gov</a> <i> updated June 3, 2004, G.Heimerdinger </i> </pre> GLOBEC Fish Larvae collected by MOCNESS nets, Standard Haul Factor: numerical factor (multiplier) used to standardize catches to be expressed as number caught per 10m2 of sea surface area. Most haul factors range from 1 to 10. 10040 inventory inventory http://globec.whoi.edu/jg/serv/globec/gb/inventory.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/inventory%7D <h2 align=center>Inventory of U.S. GLOBEC Georges Bank Data</h2> This inventory uses the JGOFS data management system and the same hierachical data structure used in many other data sets to store data about the data (metadata). <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a> 10041 moc10data moc10data http://globec.whoi.edu/jg/serv/globec/gb/moc10data_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/moc10data%7D <h2 align=center> Organism abundance derived from sampling by the <br>10 m² MOCNESS system</h2> <p><b>Important information:</b><br> <ul> <li>The catch from each net was subsampled and <u>all</u> animals in the subsample were counted. </li> <li>Due to the shear volume of data, only those animals found were represented in these on-line data. <i>i.e.</i>, no animals with zero abundances were listed. </li> <li>The precision variation in the latitude and longitude numbers is as reported. </li> <li>Not all nets for all tows are represented here. Some nets came back empty. </li> </ul> </p> <p><b>NOTE: </b>See the companion file containing the length measurements of the organisms screened. <a href="http://globec.whoi.edu/jg/serv/globec/gb/moc10data_lengths_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/moc10data_lengths%7D"> moc10data lengths</a></p> <pre> <b>Any questions, contact:</b><i> Erich Horgan Woods Hole Oceanographic Institution Woods Hole, MA 02543 voice: (508) 289-3207 fax: (508) 457-2169 e-mail: <a href="mailto:ehorgan@whoi.edu">ehorgan@whoi.edu</a> <i>December 2, 2005 mda</i> </i> </p> </pre> Zooplankton Data from the 10m2 MOCNESS. <ul> <li>The catch from each net was subsampled and <u>all</u> animals in the subsample were counted. </li> <li>Due to the shear volume of data, only those animals found were represented in these on-line data. <i>i.e.</i>, no animals with zero abundances were listed. </li> <li>The precision variation in the latitude and longitude numbers is as reported. </li> <li>Not all nets for all tows are represented here. Some nets came back empty. </li> </ul> 10042 moc10data_lengths moc10data_lengths http://globec.whoi.edu/jg/serv/globec/gb/moc10data_lengths_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/moc10data_lengths%7D <h2 align=center> Organism lengths, <br> samples obtained by the 10 m² MOCNESS system</h2> <p><b>Note: </b> See companion file containing abundance and additional tow info. <a href="http://globec.whoi.edu/jg/serv/globec/gb/moc10data_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/moc10data%7D"> moc10data zooplankton abundance</a></p> <pre> <b>Any questions, contact:</b><i> Erich Horgan Woods Hole Oceanographic Institution Woods Hole, MA 02543 voice: (508) 289-3207 fax: (508) 457-2169 e-mail: <a href="mailto:ehorgan@whoi.edu">ehorgan@whoi.edu</a> <i>December 27, 2005 mda</i> </i> </p> </pre> Moc 10 zooplankton length data, <ul> <li>The catch from each net was subsampled and <u>all</u> animals in the subsample were counted. </li> <li>Due to the shear volume of data, only those animals found were represented in these on-line data. <i>i.e.</i>, no animals with zero abundances were listed. </li> <li>The precision variation in the latitude and longitude numbers is as reported. </li> <li>Not all nets for all tows are represented here. Some nets came back empty. </li> </ul> 10043 mocness_ctd mocness_ctd http://globec.whoi.edu/jg/serv/globec/gb/ctd_mocness.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/mocness_ctd%7D <p> The MOCNESS is based on the Tucker Trawl principle (Tucker, 1951). The particular MOCNESS system from which these CTD data came is one of three net systems. The MOCNESS-1 has nine rectangular nets (1m x 1.4 m) which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976). The MOCNESS-10 (with 10 m² nets)carries 6 nets of 3.0-mm circular mesh. The MOCNESS-.25 carries nine rectangular nets (1/4-m²), usually with 64 micrometer mesh. In all three systems, "the underwater unit sends a data frame, comprised of temperature, depth, conductivity, net-frame angle, flow count, time, number of open net, and net opening/closing, to the deck unit in a compressed hexadecimal format every 2 seconds and from the deck unit to a microcomputer every 4 seconds... Temperature (to approximately 0.01 deg C) and conductivity are measured with SEABIRD sensors. Normally, a modified T.S.K.-flowmeter is used... Both the temperature and conductivity sensors and the flowmeter are mounted on top of the frame so that they face horizontally when the frame is at a towing angle of 45deg... Calculations of salinity (to approximately 0.01 o/oo S), potential temperature (theta), potential density (sigma), the oblique and vertical velocities of the net, and the approximate volume filtered by each net are made after each string of data has been received by the computer." (Wiebe <i>et al.</i>, 1985) In addition, data were collected from four other sensors attached to the frame: the Transmissometer, the Fluorometer, the Downwelling light sensor, and the Oxygen sensor. A SeaBird underwater pump was also included in the sensor suite. </p> <p><b> It should be noted that whenever the data are of questionable value, "50.000" is written in the particular data field. </b> </p> <p><u>The following notes are cruise-specific:</u><br> <b>OC319:</b> Lats and Lons for first two tows are missing because gps string not yet available.</p> <p>Unless otherwise indicated, these data have not been post-processed.</p> <p>For additional information, contact the <a href="http://usjgofs.whoi.edu/jg/serv/globec/gb/inventory.html0?project,name_prin"> chief scientist</a> for the cruise or the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">U.S. GLOBEC Data Management Office</a> (DMO). </p> <p> <b>Note:</b> Some variables have been eliminated from the display but are nevertheless available. These variables include: oxycurrent, oxytemp, tempco, and echo.</p> <p> <h2>References</h2> ¹Fofonoff and Millard, 1983, UNESCO technical papers in Marine Sciences, #44 </p> <p> Tucker, G.H., 1951. Relation of fishes and other organisms to the scattering of underwater sound. <i> Journal of Marine Research</i>, <b>10:</b> 215-238. </p> <p> Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. <i>Journal of Marine Research</i>, <b>34(3):</b> 313-326 </p> <p> Wiebe, P.H., A.W. Morton, A.M. Bradley, R.H. Backus, J.E. Craddock, V. Barber, T.J. Cowles and G.R. Flierl, 1985. New developments in the MOCNESS, an apparatus for sampling zooplankton and micronekton. <i>Marine Biology</i>, <b>87:</b> 313-323. </p> <i> updated October 27 2005, gfh</i> </pre> 10044 nut_phyto nut_phyto http://grampus.umeoce.maine.edu/jg/serv/globec/nut_phyto.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/nut_phyto%7D <h4 align=center> Phytoplankton Chlorophyll and Nutrient Studies<br> on Georges Bank<br> David W. Townsend, Keska Kemper, Maura A. Thomas, <br> Annette L. Brickley and Abigail M. Deitz </h4> <h4><i>PROJECT OVERVIEW:</i></h4> The project began in the winter of 1997 as part of the <a href="http://globec.whoi.edu">U.S. GLOBEC Georges Bank Program</a>. The purpose of our component of that multi-institutional study is to investigate the idea that the growth and production of zooplankton and fish on Georges Bank are limited by the amount of nutrients (especially nitrogen) that is brought onto the Bank from the nutrient-rich, deeper waters around the Bank's edges (cf. Townsend and Pettigrew, 1997). <p> <p> The sampling period was chosen to bracket the winter-to-spring transition, which is coincident with the Georges Bank GLOBEC broad scale cruises conducted in 1997, 1998 and 1999. The cruise dates were: <p> <pre> 1997*January 13 - 20 (R/V Albatross) *February 11 - 22 (R/V Oceanus) *March 16 - 29 (R/V Oceanus) *April 20 - May 3 (R/V Oceanus) *May 19 - 30 (R/V Oceanus) *June 18 - 28 (R/V Albatross) 1998*February 7 -17 (R/V Oceanus) *March15 - 26 (R/V Oceanus) *April 16 - 26 (R/V Oceanus) *May 10 - 20 (R/V Albatross) *June 17 - 25 (R/V Albatross) 1999*January 11 - 24 (R/V Albatross) *February 11 - 23 (R/V Oceanus) *March 10 - 23 (R/V Endeavor) *April 16 - 28 (R/V Oceanus) *May 19 - 27 (R/V Albatross) *June 14 - 24 (R/V Albatross) </pre> <p> Water samples were collected on all cruises for the analysis of phytoplankton biomass (chlorophyll a and phaeophytin). In addition, dissolved inorganic nutrient concentrations (NO3+NO2, SiO4, PO4 and NH4) were determined for four of the six Broadscale cruises in 1997, five of six in 1998, and all six in 1999. Water collections were made at various depths at all of the regular hydrographic stations (1-40 or Sta 41 after 1997) using Niskin bottles mounted on the rosette sampler. Additional surface water samples were collected at positions between the regular stations (numbered &gt;41; refer to <a href="http://globec.whoi.edu/images/station_locations_townsend.gif"> Station Location Map</a> for example). Note that because data files are in some cases ordered by station number, time does not necessarily increase monotonically throughout a given data file. Detection limits for ammonia vary for each month of analysis; for details contact Maura Thomas (mthomas@maine.edu) or David Townsend (davidt@maine.edu). <p> Phytoplankton chlorophyll a and phaeopigments were determined fluorometrically (Parsons et al., 1984). The extracted chlorophyll measurements involved collecting 100ml from all bottle samples taken at depths shallower than 60m, filtering through GF/F filters, and extracting in 90% acetone in a freezer for at least 12 hours. The samples were analyzed at sea using a Turner Model 10 fluorometer. <p> Water samples for DIN were filtered through 0.45 Millipore cellulose acetate membrane filters and then frozen immediately in 20ml acid-washed polyethylene scintillation vials by first placing the vials in a seawater-ice bath for approximately 10 minutes. Samples were analyzed in the lab following the cruise using a Technicon II 4-Channel Auto-Analyzer. <p> In addition to dissolved inorganic nutrients and chlorophyll, in 1999 we are also analyzing samples for particulate organic carbon and nitrogen, dissolved organic nitrogen, and particulate and dissolved organic phosphorus. <p> Results from the vertical profiles taken at each station can be viewed as contour plots (using Surfer Software, Golden Colorado) for <a href="http://grampus.umeoce.maine.edu/globec/globec97/globec97.htm">1997</a>, <a href="http://grampus.umeoce.maine.edu/globec/globec98/globec98.htm">1998</a> and <a href="http://grampus.umeoce.maine.edu/globec/globec99/globec99.htm">1999</a>. Plotted variables include Temperature and Salinity for the hydrographic data, Chlorophyll a for the pigment analyses and Nitrate plus Nitrite, Silicate, Ammonium and Phosphate for the inorganic nutrient analyses. The hydrographic data were contoured only for the surface(2m). The pigment and inorganic nutrient concentrations were contoured for the surface(2m), 20meter and 60 meter depths. <p> <h4><i>REFERENCES:</i></h4> Parsons, T.R., Y. Maita and C.M. Lalli. 1984. A Manual of Chemical and Biological Methods for Seawater Analysis. Pergamon, Oxford. 173pp. <p> Townsend, D.W. and N.R. Pettigrew. 1997. Nutrient limitation of secondary production on Georges Bank. <i>J. Plankton Res.</i> 19: 221-235. <p> </pre> Phytoplankton Chlorophyll and Nutrient Studies on Georges Bank Water samples were collected on all cruises for the analysis of phytoplankton biomass (chlorophyll a and phaeophytin). In addition, dissolved inorganic nutrient concentrations (NO3+NO2, SiO4, PO4 and NH4) were determined for four of the six Broadscale cruises in 1997, five of six in 1998, and all six in 1999. Water collections were made at various depths at all of the regular hydrographic stations (1-40 or Sta 41 after 1997) using Niskin bottles mounted on the rosette sampler. Additional surface water samples were collected at positions between the regular stations (numbered >41; refer to Station Location Map for example). Note that because data files are in some cases ordered by station number, time does not necessarily increase monotonically throughout a given data file. Detection limits for ammonia vary for each month of analysis; for details contact Maura Thomas (mthomas@maine.edu) or David Townsend (davidt@maine.edu). 10045 station_plans station_plans http://globec.whoi.edu/jg/serv/globec/gb/station_plans.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/station_plans%7D The locations for the broad-scale stations are defined for all the broad-scale cruises. Each station has a priority (priority 1 is a higher priority than 2, etc.) For more detailed information about the station protocol, see <a href="http://globec.whoi.edu/globec-dir/corestations.html"> http://globec.whoi.edu/globec-dir/corestations.html</a>. <p> <pre> Parameter Description Units description description of stations n/a (maintain record of how stations have changed over time) station pre-assigned station number n/a lat_deg latitude degrees degrees lat_min latitude minutes minutes lat_ddmm.tt latitude deg. & minutes dd=degrees mm=minutes tt=fractions of minutes lon_deg longitude degrees degrees lon_min longitude minutes minutes lon_ddmm.tt longitude deg. & minutes dd=degrees mm=minutes tt=fractions of minutes lat decimal latitude decimal degrees lon decimal longitude decimal degrees depth_w water depth meters distance distance between stations nautical miles priority station priority n/a </pre> <p> The total track line is 710.9 nm <p> Note that standard station #40 is <p> <ul> <li> to take place in deep water (183m), and <li> to include a MOCNESS 10 tow, even though it is a priorty 3 station. </ul> <p> Note also that the track line to station #41 should be followed, if possible, even if the station itself will be skipped. The ADCP record along the segments is of high priority for the modeling efforts. </pre> 10046 wind_stress wind_stress http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/wind_stress.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/wind_stress%7D <h2 align=center>Wind Stress calculated for NOAA Weather Buoys,<br> Nantucket Lightship and Globec Mooring ST1</h2> <p> Wind Stress as calculated by Large & Pond (JPO, '81) where the wind is corrected to 10m elevation. <p> Matlab code ("wstr.m") & raw data available on request from Jim Manning. <p> Additional information is available in the manuscript <a href="http://www.nefsc.noaa.gov/epd/ocean/MainPage/ManningStroutWind.pdf" target=_blank> Georges Bank Winds article, as a pdf file.</a>. <p> <pre> <b>Buoy/station location history:</b> Buoy ID 44003 LAT/LON OPER. PERIOD (month/year) 40.8 N./68.5 W. 03/77-03/84 ------------------- BUOY ID 44005 LAT/LON OPER. PERIOD 42.7 N./68.3 W. 12/78-03/88 42.7 N./68.6 W. 06/88-08/91 42.6 N./68.6 W. 01/92-01/94 42.9 N./68.9 W. 04/94-03/01 43.2 N./69.2 W. 03/01-09/02 43.2 N./69.2 W. 02/03-06/03 ---------------------- Buoy ID 44008 LAT/LON OPER. PERIOD 40.5 N./69.4 W. 8/82-06/03 ---------------------- Buoy ID 44011 LAT/LON OPER. PERIOD 41.1 N./66.6 W. 05/84-05/03 ---------------------- Buoy ID 44018 LAT/LON OPER. PERIOD 41.3 N./69.3 W. 07/02-06/03 ----------------------- Nantucket Lightship (ntls) LAT/LON OPER. PERIOD 40.5 N./69.46 W. 1975-1981 ------------------------ GLOBEC mooring site ST1 LAT/LON OPER. PERIOD 40.864 N./67.558 W. 01/95-08/95 <b>Any questions, contact:</b> Jim Manning National Marine Fisheries Service, NEFC Woods Hole, MA 02543 voice: 508-495-221 fax: 508-495-2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> <i> updated: 13 July 2005, gfh</i> </pre> Wind Stress as calculated by Large & Pond (JPO, 1981) where the wind is corrected to 10m elevation. Matlab code ("wstr.m") & raw data available on request from Jim Manning. Additional information is available in the manuscript Georges Bank Winds article, as a pdf file.. <pre> BUOY ID 44005 LAT/LON OPER. PERIOD 42.7 N./68.3 W. 12/78-03/88 42.7 N./68.6 W. 06/88-08/91 42.6 N./68.6 W. 01/92-01/94 42.9 N./68.9 W. 04/94-03/01 43.2 N./69.2 W. 03/01-09/02 43.2 N./69.2 W. 02/03-06/03 </pre> 10047 vpr_cashjian vpr_cashjian http://globec.whoi.edu/jg/serv/globec/gb/vpr_cashjian.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/vpr_cashjian%7D <h2 align=center>Video Plankton Recorder Data</h2> <p> <body> <b>Methodology</b> <p>The following information was extracted from <i>C.J. Ashjian et al., Deep- Sea Research II 48(2001) 245-282 </i>. An in-depth discussion of the data and sampling methods can be found there. </p> <p>The Video Plankton Recorder was towed at 2 m/s, collecting data from the surface to the bottom (towyo). The VPR was equipped with 2-4 cameras, temperature and conductivity probes, fluorometer and transmissometer. Environmental data was collected at 0.25 Hz (CI9407) or 0.5 Hz (EN259, EN262). Video images were recorded at 60 fields per second (fps).</p> <p>Video tapes were analyzed for plankton abundances using a semi-automated method discussed in <i>Davis, C.S. et al., Deep-Sea Research II 43 (1996) 1946-1970</i>. In-focus images were extracted from the video tapes and identified by hand to particle type, taxon, or species. Plankton and particle observations were merged with environmental and navigational data by binning the observations for each category into the time intervals at which the environmental data were collected (again see above <i>Davis</i> citation). Concentrations were calculated utilizing the total volume (liters) imaged during that period. For less-abundant categories, usually only a single organism was observed during each time interval so that the resulting concentrations are close to presence or absence data rather than covering a range of values. </body></p> <pre> <b>Any questions, contact:</b> Carin Ashjian Woods Hole Oceanographic Institution Woods Hole, Ma 02540 Voice: 508-289-3457 Fax: 508-457-2169 Email: <a href="mailto:cashjian@whoi.edu">cashjian@whoi.edu</a> <i> updated: May 08, 2006 </i></pre> </p> </pre> The Video Plankton Recorder was towed at 2 m/s, collecting data from the surface to the bottom (towyo). The VPR was equipped with 2-4 cameras, temperature and conductivity probes, fluorometer and transmissometer. Environmental data was collected at 0.25 Hz (CI9407) or 0.5 Hz (EN259, EN262). Video images were recorded at 60 fields per second (fps). Video tapes were analyzed for plankton abundances using a semi-automated method discussed in Davis, C.S. et al., Deep-Sea Research II 43 (1996) 1946-1970. In-focus images were extracted from the video tapes and identified by hand to particle type, taxon, or species. Plankton and particle observations were merged with environmental and navigational data by binning the observations for each category into the time intervals at which the environmental data were collected (again see above Davis citation). Concentrations were calculated utilizing the total volume (liters) imaged during that period. For less-abundant categories, usually only a single organism was observed during each time interval so that the resulting concentrations are close to presence or absence data rather than covering a range of values. 10048 zoo_pump zoo_pump http://globec.whoi.edu/jg/serv/globec/gb/zoo_pump.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/zoo_pump%7D <h3 align=center>Zooplankton Densities/Abundance</h3> <b>Principal Investigator:</b> Lewis S. Incze <a href="mailto:lincze@usm.maine.edu">(lincze@usm.maine.edu)</a><br> <b>Research Technicians:</b> Ford Dye, Beth Novak, Nicholas Wolff<br> <p> <b>Methods:</b> <p> Using a pumping system appended to the CTD unit, measured water volumes (typically 40 liters) were sampled at descrete depths and filtered through 40 micron mesh prior to sorting. A subsample of the filtered sample was used for the zooplankton counts and identification. The size of the subsample varied and depended on the amount of zooplankton present - subsamples were larger when there were fewer animals. <p> From the subsamples, all zooplankton were counted and identifed. Counts were then converted into number per cubic meter as follows: Number counted / (Subsample size X Amount filtered). <p> It is worth noting that the frequency of repeated densities is an artifact of the small subsample volumes screened in order to process a large number of samples. The small sample volumes did not give us the ability to resolve small differences in abundance at individual species and stages (e.g., Cal fin Nauplius I). At this level of sorting many counts were reported as zeros, ones, twos or threes. These counts are at the threshold for detection, and the results give the false impression of many identical densities (concentrations). This also shows up in gaps in the life histories as well. For example, a single depth/station might have NI and NIII and NIV stages, but not II or V. As a result, samples were often recombined to give the population characteristics of an integrated water column, or a group of samples. The approach worked well for our research objectives and we are well aware of its limitations. A single station and depth in our data can be deceiving and does not tell the whole story. </p><p> <b>Note:</b> Sampling for cruise EL9904, events EL10999.24 and EL111299.6 are intentional replication sites. All sampling was made at same depth level. These stations were used to test the repeatability of methods. </p> <p> <b>Cruises</b> <ul> <li>SJ9508 (Seward Johnson Cruise 9508 to Southwest Georges Bank, 6 - 16 June 1995)</li> <li>OC303 (Oceanus Cruise 303 to Georges Bank, 6 - 23 May 1997)</li> <li>EL9904 (Edwin Link Cruise 9904 to Georges Bank, 14 - 28 April 1999)</li> <li>EL9905 (Edwin Link Cruise 9905 to Georges Bank, 10 - 29 May 1999)</li> </ul> </p> <pre><b> Any questions, contact:</b> Lewis S. Incze University of Southern Maine P.O. Box 9300 96 Falmouth Street Portland, ME 04104-9300 Voice: 207 228 8070 Fax: 207 228 8057 Email: <a href="mailto:lincze@usm.maine.edu">(lincze@usm.maine.edu)</a> <i> updated: 23 November 2004; gfh</i> </pre> Using a pumping system appended to the CTD unit, measured water volumes (typically 40 liters) were sampled at descrete depths and filtered through 40 micron mesh prior to sorting. A subsample of the filtered sample was used for the zooplankton counts and identification. The size of the subsample varied and depended on the amount of zooplankton present - subsamples were larger when there were fewer animals. From the subsamples, all zooplankton were counted and identifed. Counts were then converted into number per cubic meter as follows: Number counted / (Subsample size X Amount filtered). <p> It is worth noting that the frequency of repeated densities is an artifact of the small subsample volumes screened in order to process a large number of samples. The small sample volumes did not give us the ability to resolve small differences in abundance at individual species and stages (e.g., Cal fin Nauplius I). At this level of sorting many counts were reported as zeros, ones, twos or threes. These counts are at the threshold for detection, and the results give the false impression of many identical densities (concentrations). This also shows up in gaps in the life histories as well. For example, a single depth/station might have NI and NIII and NIV stages, but not II or V. As a result, samples were often recombined to give the population characteristics of an integrated water column, or a group of samples. The approach worked well for our research objectives and we are well aware of its limitations. A single station and depth in our data can be deceiving and does not tell the whole story. </p> 10049 zoo_cubic_meter zoo_cubic_meter http://globec.whoi.edu/jg/serv/globec/gb/zoo_cubic_meter.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/zoo_cubic_meter%7D <h4 align=center>Zooplankton Meter³ Data</h4> The Zooplankton Meter³ Database for the Georges Bank Globec project is located in the laboratory of Ted Durbin at the Graduate School of Oceanography, University of Rhode Island. It is accessed via the U.S. GLOBEC Georges Bank data management system using SQLPlus network access to the data base management system at URI, but for performance reasons, data are cached and reserved from the local computer. <p> The Oracle data base at URI is constructed and maintained in Oracle and operates from a windows NT environment. <p> A description of the URI database is or will be available online and includes the design and variable definitions. A version of this document is shown <a href="http://globec.whoi.edu/globec-dir/data_doc/zoo_cubic_meter_URI.html">here</a>. <p> The zooplankton data are available directly from GSO's GLOBEC web site at <a href="http://globec.gso.uri.edu/"> http://globec.gso.uri.edu/</a>. <p> Additional information on this data base can be obtained by contacting Peter Garrahan by email at petebob@gso.uri.edu. <p> <b>Note:</b>Our program's<a href="http://globec.whoi.edu/globec-dir/data-acknowledgement-policy.html"> Data Acknowledgement Policy</a> requires that any person making substantial use of a data set must communicate with the investigators who acquired the data prior to publication and anticipate that the data collectors will be co-authors of published results. <p> <h3>The following documentation applies to the data found locally on the WHOI Globec Data Server.</h3> <P><font size="+2">T</font>he database is designed as a hierarchy. The least changing variables are in higher order tables (e.g., cruise id, year, month, etc.), while variables that change the most are in the lower order tables (e.g., time of collection, net number, taxon collected, etc.) There are five levels within the database; variable names and descriptions are given in the following tables. The information in the relational database is contained in the header at each level so that all relevant data is available at all levels. </P> <P><font size="+2">M</font>ost column variable names and instrument names were taken from the U.S. GLOBEC Georges Bank data thesaurus; those that were not follow the GLOBEC data protocols. The taxonomic code variable (taxon_code) is from the National Oceanographic Data Center's Taxonomic List, version 8. Taxonomic information is built into these ten-digit codes as they reflect the systematic nomenclature.</P> <p align=left> You may contact the <a href="http://usjgofs.whoi.edu/globec-dir/contact_dmo.html">U.S. GLOBEC Georges Bank Data Management Office</a> for additional help. </p></pre> The Zooplankton Meter3 Database for the Georges Bank Globec project is located in the laboratory of Ted Durbin at the Graduate School of Oceanography, University of Rhode Island. It is accessed via the U.S. GLOBEC Georges Bank data management system using SQLPlus network access to the data base management system at URI, but for performance reasons, data are cached and reserved from the local computer. 10050 zoo_square_meter zoo_square_meter http://globec.whoi.edu/jg/serv/globec/gb/zoo_square_meter.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/zoo_square_meter%7D <h4 align=center>Zooplankton Meter² Data</h4> The Zooplankton Meter² Database for the Georges Bank Globec project is located in the laboratory of Ted Durbin at the Graduate School of Oceanography, University of Rhode Island. It is accessed via the U.S. GLOBEC Georges Bank data management system using SQLPlus network access to the data base management system at URI, but for performance reasons, data are cached and reserved from the local computer. <p> The Oracle data base at URI is constructed and maintained in Oracle and operates from a windows NT environment. <p> A description of the URI database is or will be available online and includes the design and variable definitions. A version of this document is shown <a href="http://globec.whoi.edu/jg/info/globec/gb/zoo_square_meter_URI{dir=globec.whoi.edu/jg/dir/globec/gb/,data=globec.whoi.edu/jg/serv/globec/gb/zoo_square_meter.html0}">here</a>. <p> The zooplankton data are available directly from GSO's GLOBEC web site at <a href="http://globec.gso.uri.edu/"> http://globec.gso.uri.edu/</a>. <p> Additional information on this data base can be obtained by contacting Peter Garrahan by email at petebob@gso.uri.edu. <p> <b>Note:</b>Our program's<a href="http://globec.whoi.edu/globec-dir/data-acknowledgement-policy.html"> Data Acknowledgement Policy</a> requires that any person making substantial use of a data set must communicate with the investigators who acquired the data prior to publication and anticipate that the data collectors will be co-authors of published results. <p> <h3>The following documentation applies to the data found locally on the WHOI Globec Data Server.</h3> <P><font size="+2">T</font>he database is designed as a hierarchy. The least changing variables are in higher order tables (e.g., cruise id, year, month, etc.), while variables that change the most are in the lower order tables (e.g., time of collection, net number, taxon collected, etc.) There are five levels within the database; variable names and descriptions are given in the following tables. The information in the relational database is contained in the header at each level so that all relevant data is available at all levels. </P> <P><font size="+2">M</font>ost column variable names and instrument names were taken from the U.S. GLOBEC Georges Bank data thesaurus; those that were not follow the GLOBEC data protocols. The taxonomic code variable (taxon_code) is from the National Oceanographic Data Center's Taxonomic List, version 8. Taxonomic information is built into these ten-digit codes as they reflect the systematic nomenclature.</P> <p> You may contact the <a href="http://usjgofs.whoi.edu/globec-dir/contact_dmo.html">U.S. GLOBEC Georges Bank Data Management Office</a> for additional help. </p></pre> GSO/URI meter squared data. The Zooplankton Meter2 Database for the Georges Bank Globec project is located in the laboratory of Ted Durbin at the Graduate School of Oceanography, University of Rhode Island. It is accessed via the U.S. GLOBEC Georges Bank data management system using SQLPlus network access to the data base management system at URI, but for performance reasons, data are cached and reserved from the local computer. 10051 DIF_records DIF_records http://globec.whoi.edu/jg/serv/globec/gb/dif_records.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/,info=globec.whoi.edu/jg/info/globec/gb/DIF_records%7D <h3 align=center> DIF records </h3> <p>Metadata has been submitted to the <a href="http://gcmd.gsfc.nasa.gov/">Global Change Master Directory</a> as part of the grantee obligation.</p> <p>In general, any metadata record can be accessed directly through the URL:<br> http://gcmd.nasa.gov/getdif.htm?[entry_id]</p> where [entry_id] = the Entry_ID of the metadata record, e.g. wind_stress_GB</p> 10052 nepsst nepsst http://globec.coas.oregonstate.edu/jg/serv/globec/nep/nepsst.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/nepsst%7D <h4>NEP AVHRR Sea Surface Temperature Archive Web Site</h4> <p>At this website, one can view satellite fields over the regions of interest to the U.S. GLOBEC North-East Pacific (NEP) program (<a href="http://zanclopus.biol.berkeley.edu/lab/globec/globec.html"> http://zanclopus.biol.berkeley.edu/lab/globec/globec.html</a>). Funding to create and maintain this web site is provided by NSF (Ocean Sciences - Biological Oceanography) and NASA (Earth Science Enterprise - Biological Oceanography).The viewable satellite fields will eventually include: <ol> <li> Sea Surface Temperature (SST) from the NOAA AVHRR sensors over three regions - the California Current System (CCS), the coastal Gulf of Alaska (CGOA) and the entire NE Pacific, (NEP) with 1km, 3km and 9km resolutions; <li> surface pigment concentrations from the SeaWiFS sensor over the CCS and CGOA with 4km resolution; <li> gridded surface height fields from altimeters over the entire NEP and specific regions, with resolutions to be determined by requests for specific applications. </ol> <p>At present, only AVHRR SST data are available: 9-km resolution Pathfinder fields over the entire NEP and 1-3km resolution fields over the CCS (see below).Actual access of the data is through anonymous ftp at <a href="ftp://pisco.oce.orst.edu/ebc"> ftp://pisco.oce.orst.edu/ebc</a> To read more about the ftp site: <a href="http://pisco.coas.oregonstate.edu/globec/AAGBCREADME.TXT">AAGBCREADME.TXT</a> <p> Other environmental data of interest to U.S. GLOBEC NEP researchers (coastal winds, temperatures, sea levels, upwelling indices, etc., are available on the website maintained by the Pacific Environmental Fisheries Laboratory (<a href="http://www.pfeg.noaa.gov/index.html"> http://www.pfeg.noaa.gov/index.html</a>). </pre> <p> All Images from dates earlier than July 1, 2005 have been processed and navigated by Ocean Imaging of Solana Beach, CA <p> Images dated July 1, 2005 and later are generously provided by Dave Foley of NOAA Pacific Fisheries Environmental Laboratory. <p> Images are mapped to a simple rectangular grid, so each pixel represents a constant area in degrees longitude and latitude. The images begin in the northwest corner and are stored top down. Element (1,1) is the north west corner, element (1,512) is the north east corner, element (512,1) is south west and (512,512) is south east. <p> There are usually 2 AVHRR satellites passing over the west coast of N. America, making available 2 - 4 images per day for any given area. After July 1, 2005, more than 3-4 images may be present since any data capture with data in the area of interest is included. <p> For the old-style EBC California current images described under 3., only images which were judged to contain useful cloud-free areas are archived; rarely do all images from a given day meet this criterion. <p> For images dated earler than July 1, 2005: When the coast is visible, Ocean Imaging is supposed to be correcting the navigation to within 1 pixel using known coastal points, although some of the images have larger errors. These are often cloudy or foggy near the coast, making an exact determination of the coast location difficult. 10053 birds birds http://globec.whoi.edu/jg/serv/globec/nep/birds.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/birds%7D Birds from NEP NCC, R/V New Horizon <h2 align=center>GLOBEC NEP Northern California Current Bird Data<br> R/V New Horizon cruises NH0005 and 0007</h2> <p> <b>NOTES:</b><br><br> 1..Please see companion file named "metabirds", this web site. Supporting data for Bird Observations<br><br> 2..The following documentation is extracted from:<br><br> David G. Ainley, Larry B. Spear, Cynthia T. Tynan, John A. Barth, Stephen D. Pierce, R. Glenn Ford and Timothy J. Cowles, 2005. Physical and biological variables affecting seabird distributions during the upwelling season of the northern California Current. Deep Sea Research Part II: Topical Studies in Oceanography, Volume 52, Issues 1-2, January 2005, Pages 123-143 <br><br> As a part of the GLOBEC-Northeast Pacific project, we investigated variation in the abundance of marine birds in the context of biological and physical habitat conditions in the northern portion of the California Current System (CCS) during cruises during the upwelling season 2000. Continuous surveys of seabirds were conducted simultaneously in June (onset of upwelling) and August (mature phase of upwelling).<br><br> Seabird surveys were conducted continuously during daylight, using a 300-m-wide transect strip. Within that strip, birds were counted that occurred within the 90 degree quadrant off the ship's bow that offered the best observation conditions.<br><br> Observed counts of seabirds recorded as flying in a steady direction were adjusted for the effect of flight speed and direction relative to that of the ship (Spear et al., 1992; Spear and Ainley, 1997b). The effect of such flux is the most serious bias encountered during seabird surveys at sea (Spear et al., 2005). Known as random directional movement (as opposed to nonrandom directional movement, which occurs when birds are attracted or repelled from the survey vessel), this problem usually results in density overestimation because most species fly faster than survey vessels; densities of birds that fly slower or at a similar speed as the survey vessel (e.g., storm-petrels), or are flying in the same direction, are usually underestimated (Spear et al., 1992)<br><br> 3..Caution. Wind speed and direction may not be corrected for ship motion.<br><br> 4..Additional documentation, in the form of references, was provided by Dr. Ainley. <pre> L.B. Spear, N. Nur & D.G. Ainley. 1992. Estimating absolute densities of flying seabirds using analyses of relative movement. Auk 109:385-389. L.B. Spear & D.G. Ainley. 1997. Flight behaviour of seabirds in relation to wind direction and wing morphology. Ibis 139: 221-233. L.B. Spear & D.G. Ainley. 1997. Flight speed of seabirds in relation to wind speed and direction. Ibis 139: 234-251. L.B. Spear, D.G. Ainley, B.D. Hardesty, S.N.G. Howell & S.G. Webb. 2004. Reducing biases affecting at-sea surveys of seabirds: use of multiple observer teams. Marine Ornithology 32: 147?157. </pre> <p> <table border cellspacing0 cellpadding5> <caption><b>Species Codes</b></caption> <tr><th>Code</th><th>Description</th></tr> <tr><td>AKCA </td> <td> Cassin's Auklet</td></tr> <tr><td>AKPA </td> <td> Parakeet Auklet</td></tr> <tr><td>AKRH </td> <td> Rhinoceros Auklet</td></tr> <tr><td>ALBF </td> <td> Black-footed Albatross</td></tr> <tr><td>ALLA </td> <td> Laysan Albatross</td></tr> <tr><td>COBR </td> <td> Brandt's Cormorant</td></tr> <tr><td>COPE </td> <td> Pelagic Cormorant</td></tr> <tr><td>FUNO </td> <td> Northern Fulmar</td></tr> <tr><td>GUCA</td> <td> California Gull</td></tr> <tr><td>GUGW </td> <td> Glaucous-winged Gull</td></tr> <tr><td>GUHR</td> <td> Heermann's Gull</td></tr> <tr><td>GUPI </td> <td> Pigeon Guillemot</td></tr> <tr><td>GURB </td> <td> Ring-bill Gull</td></tr> <tr><td>GUSA</td> <td> Sabine's Gull</td></tr> <tr><td>GUWE </td> <td> Western Gull</td></tr> <tr><td>JALT</td> <td> Long-tailed Jaeger</td></tr> <tr><td>JAPA </td> <td> Parasitic Jaeger</td></tr> <tr><td>JAPO </td> <td> Pomarine Jaeger</td></tr> <tr><td>LOAR </td> <td> Pacific Loon</td></tr> <tr><td>LOCO</td> <td> Common Loon</td></tr> <tr><td>MUCO </td> <td> Common Murre</td></tr> <tr><td>MUMA</td> <td> Marbled Murrelet</td></tr> <tr><td>MUXA </td> <td> Xantus' Murrelet</td></tr> <tr><td>PELB </td> <td> Brown Pelican</td></tr> <tr><td>PHNO </td> <td> Red-necked Phalarope</td></tr> <tr><td>PHRE </td> <td> Red Phalarope</td></tr> <tr><td>SHFF</td> <td> Flesh-footed Shearwater</td></tr> <tr><td>SHPF</td> <td> Pink-footed Shearwater</td></tr> <tr><td>SHSO</td> <td> Sooty Shearwater</td></tr> <tr><td>SKMA </td> <td> South Polar Skua</td></tr> <tr><td>STFT</td> <td> Fork-tailed Storm-Petrel</td></tr> <tr><td>STLE</td> <td> Leach's Storm-Petrel</td></tr> <tr><td>TEAR</td> <td> Arctic Tern</td></tr> </table> </p> <p> <table border cellspacing0 cellpadding5> <caption><b>Behavior Codes</b></caption> <tr><th>Code</th><th>Description</th></tr> <tr><td> 1</td> <td>Flying directionally</td></tr> <tr><td> 2</td> <td>Sitting on water</td></tr> <tr><td> 3</td> <td>Feeding</td></tr> </table> <p> Any questions about the data, please contact the PIs:<br> David G. Ainley: <a href="mailto:dainley@sbcglobal.net">dainley@penguinscience.com</a><br> Cyndy Tynan: <a href="mailto:ctynan@sbcglobal.net">ctynan@whoi.edu</a> </p> <i>updated Sept 08. 2005; gfh</i> </pre> Seabird surveys were conducted continuously during daylight, using a 300-m-wide transect strip. Within that strip, birds were counted that occurred within the 90 degree quadrant off the ship's bow that offered the best observation conditions. Observed counts of seabirds recorded as flying in a steady direction were adjusted for the effect of flight speed and direction relative to that of the ship (Spear et al., 1992; Spear and Ainley, 1997b). The effect of such flux is the most serious bias encountered during seabird surveys at sea (Spear et al., 2005). Known as random directional movement (as opposed to nonrandom directional movement, which occurs when birds are attracted or repelled from the survey vessel), this problem usually results in density overestimation because most species fly faster than survey vessels; densities of birds that fly slower or at a similar speed as the survey vessel (e.g., storm-petrels), or are flying in the same direction, are usually underestimated (Spear et al., 1992) 10054 metabirds metabirds http://globec.whoi.edu/jg/serv/globec/nep/metabirds.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/metabirds%7D <h2 align=center>GLOBEC NEP Northern California Current Bird MetaData<br> R/V New Horizon cruises NH0005 and 0007</h2> <p> These data provide background environmental data in support of the bird data. </p> <p> <b>Caution:</b> Wind speed and direction may not be corrected for ship motion. <p> Any questions about the data, please contact the PIs:<br> David G. Ainley: <a href="mailto:dainley@sbcglobal.net">dainley@penguinscience.com</a><br> Cyndy Tynan: <a href="mailto:ctynan@sbcglobal.net">ctynan@whoi.edu</a> <p> <i>Updated Sept 13, 2005; gfh</i> </p> Seabird surveys were conducted continuously during daylight, using a 300-m-wide transect strip. Within that strip, birds were counted that occurred within the 90 degree quadrant off the ship&#039;s bow that offered the best observation conditions. Observed counts of seabirds recorded as flying in a steady direction were adjusted for the effect of flight speed and direction relative to that of the ship (Spear et al., 1992; Spear and Ainley, 1997b). The effect of such flux is the most serious bias encountered during seabird surveys at sea (Spear et al., 2005). Known as random directional movement (as opposed to nonrandom directional movement, which occurs when birds are attracted or repelled from the survey vessel), this problem usually results in density overestimation because most species fly faster than survey vessels; densities of birds that fly slower or at a similar speed as the survey vessel (e.g., storm-petrels), or are flying in the same direction, are usually underestimated (Spear et al., 1992) 10055 cetaceans cetaceans http://globec.whoi.edu/jg/serv/globec/nep/cetaceans.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/cetaceans%7D Cetacean observations from NEP NCC, R/V New Horizon <h3 align=center>GLOBEC NEP Northern California Current Cetacean Survey Data<br> R/V New Horizon cruises NH0005 and 0007</h3> <h4 align=center>Explanations of Variables</h4> <p> <p style="text-indent:0.25in">Line-transect surveys of cetaceans were conducted during two cruises of the GLOBEC Northeast Pacific Northern California Current (NCC) program in 2000: May 29 -June 13 and July 27 - August 12. ¬  Surveys were conducted across the shelf and slope off Oregon and northern California (41.9Ôؽ - 44.65Ôؽ N) from the coast to ~125.5ÔؽW. ¬  Surveys were conducted in passing mode while the <i>R/V New Horizon</i> was in transit between stations for hydrographic and zooplankton sampling. ¬  Observations were conducted from the flying bridge during daylight (~0600 to 2030) whenever sufficient visibility (i.e., > 2 nm) and weather (i.e., < Beaufort 6) allowed. ¬  Two observers simultaneously surveyed to the horizon with 25 x 150 binoculars, equipped with compass and reticle. ¬  Each observer surveyed a 100Ôؽ arc from 10Ôؽ off the bow (opposite side) to 90Ôؽ on their side of the ship. ¬  A third observer focused on the track-line by eye, aided with 7 x 50 hand-held binoculars. ¬  Sightings were entered immediately on a laptop computer connected to the ship's GPS system. ¬  Positions of all sightings were corrected to reflect the actual location of the cetaceans, rather than the ship's position. ¬  The height from the surface of the water to the eyes of observers on the 25 x 150 binoculars was 10.87 m. <br> <p>For additional information please see the following publication:<br><p> Cynthia T. Tynan, David G. Ainley, John A. Barth, Timothy J. Cowles, Stephen D. Pierce and Larry B. Spear, 2005. Cetacean distributions relative to ocean processes in the northern California Current System Deep Sea Research Part II: Topical Studies in Oceanography, Volume 52, Issues 1-2, January 2005, Pages 145-167 </p> <p> Any questions, contact PIs: <br> <p> <a href="http://www.whoi.edu/science/PO/dept/personnel/personnel_alpha_tynan.htm" target="_blank">Cynthia T. Tynan</a> <br> Woods Hole Oceanographic Institution<br> <p>David G. Ainley<br> H.T. Harvey & Associates <p> <i>updated 09/14/05, gfh</i> </p></pre> Line-transect surveys of cetaceans were conducted during two cruises of the GLOBEC Northeast Pacific Northern California Current (NCC) program in 2000: May 29 -June 13 and July 27 - August 12. Surveys were conducted across the shelf and slope off Oregon and northern California (41.9Ôؽ - 44.65Ôؽ N) from the coast to ~125.5ÔؽW. Surveys were conducted in passing mode while the R/V New Horizon was in transit between stations for hydrographic and zooplankton sampling. Observations were conducted from the flying bridge during daylight (~0600 to 2030) whenever sufficient visibility (i.e., > 2 nm) and weather (i.e., < Beaufort 6) allowed. Two observers simultaneously surveyed to the horizon with 25 x 150 binoculars, equipped with compass and reticle. Each observer surveyed a 100Ôؽ arc from 10Ôؽ off the bow (opposite side) to 90Ôؽ on their side of the ship. A third observer focused on the track-line by eye, aided with 7 x 50 hand-held binoculars. Sightings were entered immediately on a laptop computer connected to the ship's GPS system. Positions of all sightings were corrected to reflect the actual location of the cetaceans, rather than the ship's position. The height from the surface of the water to the eyes of observers on the 25 x 150 binoculars was 10.87 m. 10056 DIF_records DIF_records http://globec.whoi.edu/jg/serv/globec/nep/dif_records.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/DIF_records%7D <h3 align=center> DIF records </h3> <p>Metadata has been submitted to the <a href="http://gcmd.gsfc.nasa.gov/">Global Change Master Directory</a> as part of the grantee obligation.</p> <p>In general, any metadata record can be accessed directly through the URL:<br> http://gcmd.nasa.gov/getdif.htm?[entry_id]</p> where [entry_id] = the Entry_ID of the metadata record, e.g. wind_stress_GB</p> 10057 eventlogs eventlogs http://globec.coas.oregonstate.edu/jg/serv/globec/nep/eventlogs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/eventlogs%7D Event logs provide an overall summary of the sampling activities during a cruise. A hard copy of the event log is also included in the <a href="http://globec.whoi.edu/globec-dir/cruise-reports.html">cruise report</a>. Further documentation about event logs is available in <a href="http://globec.whoi.edu/globec-dir/require.html">Chief Scientist Data Reporting Requirements</a>. <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a><p> <p> <i>Last updated November 03, 2006; gfh</i> 10058 inventory inventory http://globec.whoi.edu/jg/serv/globec/nep/inventory.html0%7Bdir=globec.whoi.edu/jg/dir/globec/nep/,info=globec.whoi.edu/jg/info/globec/nep/inventory%7D <h3 align=center>Inventory of U.S. GLOBEC Northeast Pacific Data</h3> This inventory uses the JGOFS data management system and the same hierachical data structure used in many other data sets to store data about the data (metadata). Data fields include: <p> <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a> 10059 ADCP_hourly ADCP_hourly http://pleiades.esr.org/jg/serv/globec/adcp_hourly.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ADCP_hourly%7D <h3 align=center>Southern Ocean GLOBEC Hourly ADCP Data</h3> <h4>Quality </h4> <p>The following datasets have been processed and represent fairly accurate results. However, these datasets may undergo additional editing. The user is therefore cautioned that the files listed here for download may not be the final datasets. </p> <p>If you would like to be notified when updated versions are available, email Susan Howard and you will be put on a list. Otherwise, please check back for updates. Notes on the quality of each data set are included in the downloads. </p> <h4>Format </h4> <p>The datasets have been created using MATLAB. They are converted to ASCII before serving using the JGOFS data management system. The files are also available for download in their original, zipped form. Each *.zip file contains a *.mat file and a readme.txt file. See the URL below for access to the orginal Matlab files. <h4>Single Ping Data </h4> Single ping data from all cruises have been archived, but are not yet available for distribution by ESR. <p> For additional documentation of the ADCP data collected during Southern Ocean Globec and for access to the original Matlab files, see <a href="http://www.esr.org/globec_index.html" target="_blank"> http://www.esr.org/globec_index.html</a> and <a href="http://www.esr.org/globec/adcp_data.html" target="_blank"> http://www.esr.org/globec/adcp_data.html </a>. </p> <p> <b>Questions concerning these data should be directed to:</b><br> Laurence Padman<br> Earth and Space Research Institute<br> 3350 SW Cascade Ave.<br> Corvallis, OR 97333-1536, USA<br> Phone: 541-753-6695<br> E-mail: padman@esr.org<br><br> or<br><br> Susan L. Howard<br> Earth and Space Research Institute<br> 1910 Fairview Ave. E., Suite 210<br> Seattle, WA 98102, USA<br> Phone: 360-668-6817<br> E-mail: Howard@esr.org<br><br> <i> Last updated May 1, 2007 </i> In 2001, the RVIB NB Palmer and RVIB LM Gould were upgraded to collect a full suite of data needed for full single-ping editing (i.e. processing single pings to ocean velocities). LMG0103, LMG0104, and LMG0106 were collected before the new system was implemented. The single ping data from these cruises can only be used as an aid for looking at amplitude (backscatter). NBP0103, NBP0104, NBP0202, NBP0204, LMG0201A, LMG0203, LMG0205, and LMG0302 datasets contain the complete set of data needed for processing the single ping data. <h4>Format </h4> <p>The datasets have been created using MATLAB. They are converted to ASCII before serving using the JGOFS data management system. The files are also available for download in their original, zipped form. Each *.zip file contains a *.mat file and a readme.txt file. See the URL below for access to the orginal Matlab files. </p><h4>Single Ping Data </h4> Single ping data from all cruises have been archived, but are not yet available for distribution by ESR. <p> For additional documentation of the ADCP data collected during Southern Ocean Globec and for access to the original Matlab files, see <a href="http://www.esr.org/globec_index.html" target="_blank"> http://www.esr.org/globec_index.html</a> and <a href="http://www.esr.org/globec/adcp_data.html" target="_blank"> http://www.esr.org/globec/adcp_data.html </a>. 10060 ADCP_5minute ADCP_5minute http://pleiades.esr.org/jg/serv/globec/adcp_5minute.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ADCP_5minute%7D <h3>Southern Ocean GLOBEC Five Minute ADCP Data</h3> <p> <h4>Quality </h4> <p>The following datasets have been processed and represent fairly accurate results. However, these datasets may undergo additional editing. The user is therefore cautioned that the files listed here for download may not be the final datasets. </p> <p> If you would like to be notified when updated versions are available, email Susan Howard and you will be put on a list. Otherwise, please check back for updates. Notes on the quality of each data set are included in the downloads. </p> <h4>Format </h4> <p>The datasets have been created using MATLAB. They are converted to ASCII before serving using the JGOFS data management system. The files are also available for download in their original, zipped form. Each *.zip file contains a *.mat file and a readme.txt file. See the URL below for access to the original Matlab files. </p> <p> <h4>Single Ping Data </h4> <p>Single ping data from all cruises have been archived, but are not yet available for distribution by ESR. </p> <p> For additional documentation of the ADCP data collected during Southern Ocean Globec and for access to the original Matlab files, see <a href="http://www.esr.org/globec_index.html"> http://www.esr.org/globec_index.html</a> and <a href="http://www.esr.org/globec/adcp_data.html" target="_blank"> http://www.esr.org/globec/adcp_data.html </a>. </p> <p> <b>Questions concerning these data should be directed to:</b><br> Laurence Padman<br> Earth and Space Research Institute<br> 3350 SW Cascade Ave.<br> Corvallis, OR 97333-1536, USA<br> Phone: 541-753-6695<br> E-mail: padman@esr.org<br><br> or<br><br> Susan L. Howard<br> Earth and Space Research Institute<br> 1910 Fairview Ave. E., Suite 210<br> Seattle, WA 98102, USA<br> Phone: 360-668-6817<br> E-mail: Howard@esr.org<br><br> <i> Last updated May 1, 2007</i> In 2001, the RVIB NB Palmer and RVIB LM Gould were upgraded to collect a full suite of data needed for full single-ping editing (i.e. processing single pings to ocean velocities). LMG0103, LMG0104, and LMG0106 were collected before the new system was implemented. The single ping data from these cruises can only be used as an aid for looking at amplitude (backscatter). NBP0103, NBP0104, NBP0202, NBP0204, LMG0201A, LMG0203, LMG0205, and LMG0302 datasets contain the complete set of data needed for processing the single ping data. <h4>Format </h4> <p>The datasets have been created using MATLAB. They are converted to ASCII before serving using the JGOFS data management system. The files are also available for download in their original, zipped form. Each *.zip file contains a *.mat file and a readme.txt file. See the URL below for access to the orginal Matlab files. </p><h4>Single Ping Data </h4> Single ping data from all cruises have been archived, but are not yet available for distribution by ESR. <p> For additional documentation of the ADCP data collected during Southern Ocean Globec and for access to the original Matlab files, see <a href="http://www.esr.org/globec_index.html" target="_blank"> http://www.esr.org/globec_index.html</a> and <a href="http://www.esr.org/globec/adcp_data.html" target="_blank"> http://www.esr.org/globec/adcp_data.html </a>. 10061 alongtrack alongtrack http://globec.whoi.edu/jg/serv/globec/soglobec/alongtrack.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/alongtrack%7D <h3 align = center> Environmental and Navigational Data from the Ship's Monitoring Systems,<br> Reported along the Ship's Track </h3> <p>This along track (JGOFS) data set was obtained primarily by applying calibrations to raw data and decimating to whole minute intervals. Several fields are derived measurements from more than an single raw input. For example, Course Made Good (cmg) and Speed Over Ground (sog) are calculated from gyro and GPS inputs. </p> <p>Cruises often used "9.99" or "9999" to indicate bad data. Those numbers were changed to 'nd'. Not all bad data were flagged in this way however. Users of these data are encouraged to read the Data Report (found at the Directory Level of this system under "Inventory" then under "project/cruise id", and then under "data report") in order to be aware of bad data points that are not indicated by "9"s and therefore remain in the dataset.</p> <p> <b>Questions regarding this data set should be directed to:</b><br> Bob Groman<br> GLOBEC Data Management Office<br> Woods Hole Oceanographic Inst.<br> Woods Hole, MA 02543<br><br> Phone: 508 548 1400<br> E-mail: <a href="mailto:rgroman@whoi.edu">rgroman@whoi.edu</a><br><br> <i>Last updated March 15, 2006</i> Along track data, including CTD, MET and navigation information. This along track (JGOFS) data set was obtained primarily by applying calibrations to raw data and decimating to whole minute intervals. Several fields are derived measurements from more than an single raw input. For example, Course Made Good (cmg) and Speed Over Ground (sog) are calculated from gyro and GPS inputs.Cruises often used &#039;9.99&#039; or &#039;9999&#039; to indicate bad data. Those numbers were changed to &#039;nd&#039;. Not all bad data were flagged in this way however. 10062 awsD awsD http://globec.whoi.edu/jg/serv/globec/soglobec/awsD.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/awsD%7D <h3 align=center>SO GLOBEC Moored Array, Drifter, and Float Component</h3> <p align=center>PIs: Bob Beardsley, Dick Limeburner, Breck Owen</p> <p align=center>Surface meteorological data collected at Dismal Island</p> Surface meteorological data collected at Dismal Island. <br>Location 68.09S - 68.82W, elev. 10m (source http://amrc.ssec.wisc.edu/aws/) <p>Source File: SOG_aws_rawNEW2.mat (from Mike Caruso)</p> <p>Records: 16969</p> <p>Period: Start: 05/23/2001 00 GMT<br> Stop: 04/30/2003 00 GMT</p> <p>Sample Rate: 1 hr</p> Processing by Beardsley group:<br> Edit barometric pressure, air temp., relative humidity, and wind speed by:<br> (a) removing values outside bounds, <br> (b) convert wind speed and direction (met convention) into east and north wind components u,v (ocean convention),<br> (c) removing wild points, (csub1) average resulting edited data in 1 hr time bins to create uniform hourly time series, <br> (d) truncate each variable into common time base, <br> (e) compute wind stress, sensible heat flux and latent heat flux using COARE26, with SST set to 0 and sensor height 12 m). <br> Save times tuv0 when raw wind speed = 0 (prop stuck due to icing, etc). [edit_aws_rawD.m, awsintA.m, coare26v.m] 10063 awsK awsK http://globec.whoi.edu/jg/serv/globec/soglobec/awsK.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/awsK%7D <h3 align=center>SO GLOBEC Moored Array, Drifter, and Float Component</h3> <p align=center>PIs: Bob Beardsley, Dick Limeburner, Breck Owen</p> <p align=center>Surface meteorological data collected at Kirkwood Island</p> <p align=center>Location 68.34S - 69.01W, elev 30m (source http://amrc.ssec.wisc.edu/aws/) <p align=center><b>Fieldname descriptions</b></p> <p>Date of submission: 12/07/04</p> <p>Source File: SOG_aws_rawNEW2.mat (from Mike Caruso)</p> <p>Processing by Beardsley group:<br> Edit barometric pressure, air temp., relative humidity, and wind speed by:<br> (a) removing values outside bounds, <br> (b) convert wind speed and direction (met convention) into east and north wind components u,v (ocean convention),<br> (c) removing wild points, (csub1) average resulting edited data in 1 hr time bins to create uniform hourly time series, <br> (d) truncating each variable into common time base, <br> (e) compute wind stress, sensible heat flux and latent heat flux using COARE26, with SST set to 0 and sensor height 12 m). <br> Save times tuv0 when raw wind speed = 0 (prop stuck due to icing, etc). [edit_aws_rawD.m, awsintA.m, coare26v.m] <font color = "red">(not served)</font> </p> <p>Sample Rate: 1 hr</p> <p>Records: 16993</p> <p>Period: Start: 05/22/2001 00 GMT<br> Stop: 04/30/2003 00 GMT</p> <pre> <i>Last updated March 1, 2006 </i></pre> Surface meteorological data collected at Kirkwood Island. <br>Location 68.34S - 69.01W, elev 30m (source <a href="http://amrc.ssec.wisc.edu/aws/">http://amrc.ssec.wisc.edu/aws/</a>) Processing by Beardsley group:<br> Edit barometric pressure, air temp., relative humidity, and wind speed by:<br> (a) removing values outside bounds, <br> (b) convert wind speed and direction (met convention) into east and north wind components u,v (ocean convention),<br> (c) removing wild points, (csub1) average resulting edited data in 1 hr time bins to create uniform hourly time series, <br> (d) truncating each variable into common time base, <br> (e) compute wind stress, sensible heat flux and latent heat flux using COARE26, with SST set to 0 and sensor height 12 m). <br> Save times tuv0 when raw wind speed = 0 (prop stuck due to icing, etc). [edit_aws_rawD.m, awsintA.m, coare26v.m] 10064 bacteria_ice bacteria_ice http://globec.whoi.edu/jg/serv/globec/soglobec/bacteria_ice.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bacteria_ice%7D <h2 align=center>Bacteria Abundance, Biomass and Chlorophyll <i>a</i> in Ice Cores</h2> <p> <b>NOTES:</b><br> NBP0104: Cores labelled with "DNA" were collected for DNA analysis. <pre> <b>Contributor:</b> Dr. Christian Fritsen University and Community College System of Nevada Desert Research Institute Div. of Earth and Ecosystem Sciences 2215 Raggio Parkway Reno, NV 89512 Office: 775/673-7487 </pre> <h3 align=center>BG 235 - Methods used for chlorophyll <i>a</i> (chla) analysis and bacteria biomass determination</h3> <p><b>Core Sampling techniques:</b></p> <p> Sampling methods for recovery of chlorophyll <i>a</i> and bacteria from sea ice cores follows those described in: <br> Garrison, D.L. and K.R. Buck(1986), Organism losses during ice melting: a serious bias in sea ice community studies. <i>Polar Biol.</i>, <b>6</b>:237-239. </p> <p> Recommendations for reporting were used as outlined by:<br> Horner, R. <i>et al.</i>,(1992), Ecology of Sea Ice Biota. I: Habitat, Terminology and Methodology. <i> Polar Biol.</i> <b>12</b>:417-427 </p> <p><b> Analytic Techniques:</b></p> <p>Chla (mg m^-3): <ul> <li>determined fluorometrically (Turner Designs 10AU Fluorometer) following extraction in 90% acetone (Parsons <i>et al</i>., 1984)</li> <li>ice core chla corrected to account for chla in filtered sea water (FSW) added to core sections during melting</li> </ul> <p>Bacteria cell abundance (cells m^-3) and biomass (mg C m^-3): <p>LMG 0106</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with 4',6-diamidino-2-phenylindole (DAPI; 0.1 to 0.3% final concentration), filtered through 0.2 mm black, polycarbonate membrane filters, and mounted onto glass microscope slides on the ship (within 24 hours following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³; as determined from mean length and width measurements), and an allometric conversion factor for bacterial carbon per volume specific for DAPI-stained bacteria (cellular carbon = 218 X BV^0.86; Loferer-Krößbacher <i>et al.</i>, 1998).</li> <li>ice core samples corrected for FSW dilution</li> </ul> <p>NBP 0104</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with Sybræ Gold (0.01% final concentration), filtered through 0.2 mm Anodisc filters (Whatmanæ), and mounted onto glass microscope slides at home institution (~1-2 months following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³), and an allometric conversion factor for bacterial carbon per volume specific for Acridine Orange-stained bacteria (cellular carbon = 89.9 X BV^0.59; Simon and Azam, 1989). Note: an AO-specific carbon per volume conversion factor was used in calculating biomass in Sybræ Gold-stained samples because both AO and Sybræ Gold stain bacteria cells similarly relative to DAPI (unpublished data). </li> <li>ice core samples corrected for FSW dilution</li> </ul> <p>Loferer-Krößbacher, M., Klima, J., and R. Psenner. 1998. Determination of bacterial cell dry mass by transmission electron microscopy and densitometric image analysis. Applied and Environmental Microbiology. 64:688-694.</p> <p>Parsons,T.R., Maita, Y., and C.M. Lalli. 1984. A manual of chemical and biological methods for seawater analysis. Pergamon Press. Elmsford, New York.</p> <p>Simon, M., and F. Azam. 1989. Protein content and protein synthesis rates of planktonic marine bacteria. Marine Ecology Progress Series. 51, 201-213.</p> <i>updated: April 20, 2006</i> <p> Sampling methods for recovery of chlorophyll <i>a</i> and bacteria from sea ice cores follows those described in: <br> Garrison, D.L. and K.R. Buck(1986), Organism losses during ice melting: a serious bias in sea ice community studies. <i>Polar Biol.</i>, <b>6</b>:237-239. </p> <p> Recommendations for reporting were used as outlined by:<br> Horner, R. <i>et al.</i>,(1992), Ecology of Sea Ice Biota. I: Habitat, Terminology and Methodology. <i> Polar Biol.</i> <b>12</b>:417-427 <pre> # Ice core bacteria data from Southern Ocean GLOBEC # C. Fritsen and F. Stewart # * BactAbun = bacterial abundance = cells m-3 # * BactBio = bacterial biomass = mg C m-3 = ug C l-1 # * chla = mg chla m-3 = ug chla l-1 # * sect_top_depth = depth(m) at top of core section </pre> <p> Sampling methods for recovery of chlorophyll <i>a</i> and bacteria from sea ice cores follows those described in: <br> Garrison, D.L. and K.R. Buck(1986), Organism losses during ice melting: a serious bias in sea ice community studies. <i>Polar Biol.</i>, <b>6</b>:237-239. </p> <p> Recommendations for reporting were used as outlined by:<br> Horner, R. <i>et al.</i>,(1992), Ecology of Sea Ice Biota. I: Habitat, Terminology and Methodology. <i> Polar Biol.</i> <b>12</b>:417-427 </p> <p>LMG 0106</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with 4&#039;,6-diamidino-2-phenylindole (DAPI; 0.1 to 0.3% final concentration), filtered through 0.2 mm black, polycarbonate membrane filters, and mounted onto glass microscope slides on the ship (within 24 hours following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³; as determined from mean length and width measurements), and an allometric conversion factor for bacterial carbon per volume specific for DAPI-stained bacteria (cellular carbon = 218 X BV^0.86; Loferer-Krößbacher <i>et al.</i>, 1998).</li> <li>ice core samples corrected for FSW dilution</li> </ul> <pre> # LMG0106: "a" "b" "c" labels appended to core numbers denote replicate cores. # "(1)" "(2)" "(3)" labels appended to core numbers denote different </pre> 10065 bacteria_brine bacteria_brine http://globec.whoi.edu/jg/serv/globec/soglobec/bacteria_brine.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bacteria_brine%7D <h2 align=center>Bacteria Chlorophyll <i>a</i> in Ice Brine</h2> <p> <b>Contributor:</b><br> Dr. Christian Fritsen<br> University and Community College System of Nevada <br> Desert Research Institute<br> Div. of Earth and Ecosystem Sciences<br> 2215 Raggio Parkway<br> Reno, NV 89512<br> Office: 775/673-7487</p> <p><b> Methods: </b><br> Brine samples were collected from auger holes that were drilled into sea ice using a 2 inch kovacs coring auger. Brine that flowed into the bottom of the hole was collected using a tygon tubing attached to a 60 cc syringe. Cholorophyll-a concentrations were determined using the techniques as reported in previous submissions of ice core and water column data. Multiple sample numbers reflect replicate samples taken from the same hole.</p> <p><i>updated: April 10, 2007</i></p> Brine samples were collected from auger holes that were drilled into sea ice using a 2 inch kovacs coring auger. Brine that flowed into the bottom of the hole was collected using a tygon tubing attached to a 60 cc syringe. Cholorophyll-a concentrations were determined using the techniques as reported in previous submissions of ice core and water column data. Multiple sample numbers reflect replicate samples taken from the same hole. <pre> # Ice brine chlorophyll-a concentrations from ice core holes # Southern Ocean, GLOBEC # C. Fritsen, Desert Research Institute # RVIB Nathaniel B. Palmer cruise NMP02-04, July-Sept 2002 # * chla = chlorophyll-a, micrograms per liter (ug/l) # * lat = latitude reported in decimal degrees south # * lon = longitude reportred in decimal degrees west # * bot_depth = depth to bottom of ice core hole in meters </pre> 10066 bacteria_water bacteria_water http://globec.whoi.edu/jg/serv/globec/soglobec/bacteria.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bacteria_water%7D <h2 align=center>Bacteria Abundance, Biomass and Chlorophyll <i>a</i></h2> <h2 align=center>Water Column Samples</h2> <p> <pre> <b>Contributor:</b> Dr. Christian Fritsen University and Community College System of Nevada Desert Research Institute Div. of Earth and Ecosystem Sciences 2215 Raggio Parkway Reno, NV 89512 Office: 775/673-7487 </pre> <h3 align=center>BG 235 - Methods used for chlorophyll <i>a</i> (chla) analysis and bacteria biomass determination</h3> <p><b>Core Sampling techniques:</b></p> <p> Sampling methods for recovery of chlorophyll <i>a</i> and bacteria from sea ice cores follows those described in: <br> Garrison, D.L. and K.R. Buck(1986), Organism losses during ice melting: a serious bias in sea ice community studies. <i>Polar Biol.</i>, <b>6</b>:237-239. </p> <p> Recommendations for reporting were used as outlined by:<br> Horner, R. <i>et al.</i>,(1992), Ecology of Sea Ice Biota. I: Habitat, Terminology and Methodology. <i> Polar Biol.</i> <b>12</b>:417-427 </p> <p><b> Analytic Techniques:</b></p> <p>Chla (mg m^-3): <ul> <li>determined fluorometrically (Turner Designs 10AU Fluorometer) following extraction in 90% acetone (Parsons <i>et al</i>., 1984)</li> <li>ice core chla corrected to account for chla in filtered sea water (FSW) added to core sections during melting</li> </ul> <p>Bacteria cell abundance (cells m^-3) and biomass (mg C m^-3): <p>LMG 0106</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with 4',6-diamidino-2-phenylindole (DAPI; 0.1 to 0.3% final concentration), filtered through 0.2 mm black, polycarbonate membrane filters, and mounted onto glass microscope slides on the ship (within 24 hours following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³; as determined from mean length and width measurements), and an allometric conversion factor for bacterial carbon per volume specific for DAPI-stained bacteria (cellular carbon = 218 X BV^0.86; Loferer-Krößbacher <i>et al.</i>, 1998).</li> <li>ice core samples corrected for FSW dilution</li> </ul> <p>NBP 0104</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with Sybræ Gold (0.01% final concentration), filtered through 0.2 mm Anodisc filters (Whatmanæ), and mounted onto glass microscope slides at home institution (~1-2 months following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³), and an allometric conversion factor for bacterial carbon per volume specific for Acridine Orange-stained bacteria (cellular carbon = 89.9 X BV^0.59; Simon and Azam, 1989). Note: an AO-specific carbon per volume conversion factor was used in calculating biomass in Sybræ Gold-stained samples because both AO and Sybræ Gold stain bacteria cells similarly relative to DAPI (unpublished data). </li> <li>ice core samples corrected for FSW dilution</li> </ul> <p>Loferer-Krößbacher, M., Klima, J., and R. Psenner. 1998. Determination of bacterial cell dry mass by transmission electron microscopy and densitometric image analysis. Applied and Environmental Microbiology. 64:688-694.</p> <p>Parsons,T.R., Maita, Y., and C.M. Lalli. 1984. A manual of chemical and biological methods for seawater analysis. Pergamon Press. Elmsford, New York.</p> <p>Simon, M., and F. Azam. 1989. Protein content and protein synthesis rates of planktonic marine bacteria. Marine Ecology Progress Series. 51, 201-213.</p> <p>Data from <b>LMG0106</b> (July-August, 2001) added in June 2002.</p> <p> <i>Updated: April 21, 2006</i> </pre></pre> <pre> # Bacteria data from Southern Ocean GLOBEC # C. Fritsen and F. Stewart # * BactAbun = bacterial abundance = cells m-3 # * BactBio = bacterial biomass = mg C m-3 = ug C l-1 # * chla = mg chla m-3 = ug chla l-1 </pre> Chla (mg m^-3): </p><ul> <li>determined fluorometrically (Turner Designs 10AU Fluorometer) following extraction in 90% acetone (Parsons <i>et al</i>., 1984)</li> <li>ice core chla corrected to account for chla in filtered sea water (FSW) added to core sections during melting</li> </ul> <p>Bacteria cell abundance (cells m^-3) and biomass (mg C m^-3): </p><p>LMG 0106</p> <ul> <li>preserved (0.5% glutaraldehyde) samples stained with 4&#039;,6-diamidino-2-phenylindole (DAPI; 0.1 to 0.3% final concentration), filtered through 0.2 mm black, polycarbonate membrane filters, and mounted onto glass microscope slides on the ship (within 24 hours following collection)</li> <li>bacteria enumerated using epifluorescence microscopy and sized using digital images taken with Image Pro Plus</li> <li>bacteria biomass determined using cell abundance, cell biovolume (BV; mm³; as determined from mean length and width measurements), and an allometric conversion factor for bacterial carbon per volume specific for DAPI-stained bacteria (cellular carbon = 218 X BV^0.86; Loferer-Krößbacher <i>et al.</i>, 1998).</li> <li>ice core samples corrected for FSW dilution</li> </ul> 10067 bathy bathy http://globec.whoi.edu/jg/serv/globec/soglobec/bathy.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bathy%7D <p> For description and documentation of the bathymetry data collected during Southern Ocean Globec, this will connect you to the <a href="http://www.whoi.edu/science/PO/so_globec/SO_GLOBEC_bathy.html">website </a>. </p> One objective of the SO GLOBEC program is to produce a better knowledge of the sea floor bathymetry in the program study area. Much of Marguerite Bay and the adjacent shelf was poorly charted when the program was started in 2000, so we first created a local area improved version (ETOPO8.2A) of the Sandwell and Smith ETOPO2 2-min digital gridded bathymetry for the SO GLOBEC study area. The first SO GLOBEC mooring cruise on the R/V Lawrence M. Gould in March 2001 quickly showed that the 2-min resolution of ETOPO8.2A does not resolve many of the canyons and abrupt changes in topography which characterize Marguerite Bay and the inner- to-mid shelf region, nor is it particularly accurate in even the more uniform terrain regions. <font size="3">To begin to improve this situation, high-quality swath bathymetry data were collected during both SO GLOBEC broadscale surveys using the SeaBeam system aboard the <u><i>R/VIB Nathaniel B. Palmer</i></u> in 2001. In addition, an extensive multibeam survey was conducted along the deep trough leading into Marguerite Bay aboard the <u><i>R/VIB James Clark Ross</i></u> in 2001. While the 2001 <u><i>R/VIB Nathaniel B. Palmer</i></u> SeaBeam data may need some adjustment for sound speed corrections, an initial attempt has been made to merge these new data sets with all existing center trackline and multibeam data available at the U.S. Geophysical Data Center (NGDC) or provided by other investigators. 10068 bird_effort bird_effort http://globec.whoi.edu/jg/serv/globec/soglobec/bird_effort.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bird_effort%7D <h3 align=center>Seabird Survey Effort Log</h3> <p>These data are the logistics surrounding the Bird Studies Observations, rather than the observations themselves.</p> <b>PI NOTES:</b><p> 1. Ice_Cover_Type is based on the ASPeCt (Antarctic Sea-Ice Process and Climate) classification system for sea ice and brash. Glacial ice listed as <i>bergs</i> or <i>bergy bits</i>. </p><p> 2. Time and Date can be used in conjunction with <a href="http:/jg/serv/globec/soglobec/alongtrack.html0">alongtrack</a> data to find position information. </p> <p> <table width= 30% border cellspacing=0 cellpadding=5> <caption><b>Visibility</b></caption> <tr><th>Code</th><th>Description</th></tr> <tr><td> 1</td> <td> &gt;600 m</td></tr> <tr><td> 2</td> <td>600 m</td> </tr> <tr><td> 3</td> <td>&gt;300 m</td></tr> <tr><td> 4</td> <td>300 m</td> </tr> <tr><td> 5</td> <td>&lt;300 m</td></tr> </table> <p> <b>PI Contact:</b><br> Erik Chapman<br> Old Dominion University<br> Center for Coastal Physical Oceanography<br> Norfolk, Virginia 23529<br> phone 757-377-0482<br> e-mail <a href="mailto:chapman@ccpo.odu.edu">chapman@ccpo.odu.edu</a></p> <i>Updated November 21, 2005; gfh</i></pre> </pre> These data are the logistics surrounding the Bird Studies Observations, rather than the observations themselves. <pre># Effort Log as part of the Bird Studies # Chris Ribic and Erik Chapman, SIs # Notes: N = Night; D = Day; # StartCode: 0=Start; 1=End; 0.5=change in conditions # Visibility Code = see documentation # Precipitation: 0=none; 1=fog; 2=rain; 3=snow, including sleet or hail # Cloud cover = eighths # Ice Concentration = tenths # Primary Ice cover = see documentation </pre> 10069 bird_observ bird_observ http://globec.whoi.edu/jg/serv/globec/soglobec/bird_observ.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/bird_observ%7D <h2 align=center> Seabird Survey Observations</h2><p> <b>PI Notes:</b><br> Time and Yearday can be used in conjunction with <a href="http:/jg/serv/globec/soglobec/alongtrack.html0">alongtrack</a> data to find latitude, longitude and ship's heading information. </p> <pre> <b>PI Contact:</b> Erik Chapman Old Dominion University Center for Coastal Physical Oceanography Norfolk, Virginia 23529 phone 757 377 0482 e-mail <a href="mailto:chapman@ccpo.odu.edu">chapman@ccpo.odu.edu</a> </pre><br> <a name="methods"> <p align=center> <i><b>SO GLOBEC, BG243 Predator Survey Methods </i></b></p> <p style="text-indent:0.25in">Seabird abundance and distribution within the SO GLOBEC study area was investigated using daytime and nighttime (using night vision viewers) survey work. We also recorded seal observations made within the transect area. Nighttime surveys were designed to complement daytime surveys.</p> <p><i>Daytime Surveys</i></p> <p><u>Methods</u></p> <p style="text-indent:0.25in">Strip transects were conducted simultaneously at 300 m and 600 m widths for birds. Surveys were conducted continuously while the ship was underway within the study area and when visibility was >300 m. For strip transects, two observers continuously scanned a 90&deg; area extending the transect distance (300 m and 600 m) to the side and forward along the transect line. Binoculars of 10X and 7X magnification were used to confirm species identifications. The 7X pair of binoculars also included a laser range finder. Ship followers and bird observed to be attracted to the ship were noted at first occurrence. These observations will be down-weighted in the analyses because these individuals may have been attracted to the ship from habitats at a distance from the ship. For each sighting, transect (300 m or 600 m), species, number of birds, behavior, flight direction, and any association with visible physical features, such as ice, were recorded. Distances were measured either by a range finder device as suggested by Heinemann (1981) or by the laser distance finder (when in the ice). Marine mammal sightings within the transect were also recorded.</p> <p style="text-indent:0.25in">Surveys were conducted from an outside observation post located on the port bridge wing of the <i>RVIB N.B. Palmer</i>. When it was not feasible to conduct surveys from this observation post, we surveyed from the inside port bridge wing.</p> <p><i>Seabird Nighttime Surveys</i></p> <p><u>Methods</u></p> <p style="text-indent:0.25in">ITT 200/210 Binocular Night Vision Viewers were used during one half-hour survey periods while on the survey grid. Surveys were a minimum of an hour apart. Observations were made from the bridge wing during NBP0104 and outside, from a dark area on the 01 deck, during NBP0103. Observers scanned back and forth looking for birds. Species and behavior of the bird was recorded for each observation. Observations were not conducted when visibility with the night vision viewer was less than 100 m from the ship.</p> <p align=center>Literature Cited</p> <p>Heinemann, D. 1981. A rangefinder for pelagic bird censusing. <i>J. Wildl. Manage. </i><b>45:</b>489-493.</p><br><br> <table border=1 width=70%> <caption><b>Species Codes</b></caption> <tr><th>Common Name </th><th>Code</th><th>Scientific Name</th></tr> <tr><td>Adelie Penguin </td><td>adpe </td><td> Pygoscelis adeliae </td></tr> <tr><td>Antarctic Petrel </td><td>anpe </td><td> Thalassoica antarctica </td></tr> <tr><td>Broadbilled (Antarctic) Prion </td><td>anpe </td><td> Pachyptila vittata (des.) </td></tr> <tr><td>Antarctic Tern </td><td>ante </td><td> Sterna vittata </td></tr> <tr><td>Black-browed Albatross </td><td>bbal </td><td> Diomedea melanophris </td></tr> <tr><td>Black-bellied Storm-petrel </td><td>bbsp </td><td> Fregetta tropica </td></tr> <tr><td>Imperial Shag (Blue-eyed Shag) </td><td>besh </td><td> Phalacrocorax atriceps </td></tr> <tr><td>Blue Petrel </td><td>blpe </td><td> Halobaena caerulea </td></tr> <tr><td>Antarctic (Brown) Skua </td><td>brsk </td><td> Catharacta (skua) lonnbergi </td></tr> <tr><td>Cape Petrel ('Pintado Petrel') </td><td>cape </td><td> Daption capense </td></tr> <tr><td>Chinstrap Penguin </td><td>chpe </td><td> Pygoscelis antarctica </td></tr> <tr><td>Crabeater Seal </td><td>crse </td><td> Lobodon carcinophagus </td></tr> <tr><td>Elephant Seal </td><td>else </td><td> Mirounga leonina </td></tr> <tr><td>Emperor Penguin </td><td>empe </td><td> Aptenodytes forsteri </td></tr> <tr><td>Antarctic Fur Seal </td><td>fuse </td><td> Arctocephalus gazella </td></tr> <tr><td>Grey-headed Albatross </td><td>ghal </td><td> Diomedea chrysostoma </td></tr> <tr><td>Humpback Whale </td><td>huwh </td><td> Megaptera novaeangliae </td></tr> <tr><td>Dominican Gull (Kelp Gull) </td><td>kegu </td><td> Larus dominicanus </td></tr> <tr><td>Leopard Seal </td><td>lese </td><td> Hydrurga leptonyx </td></tr> <tr><td>Minke Whale </td><td>miwh </td><td> Balaenoptera acutorostrata </td></tr> <tr><td>Ross Seal </td><td>rose </td><td> Ommatophoca rossi </td></tr> <tr><td>Southern Giant Petrel </td><td>sgpe </td><td> Macronectes giganteus </td></tr> <tr><td>Snow Petrel </td><td>snpe </td><td> Pagodroma nivea </td></tr> <tr><td>Southern Fulmar </td><td>sofu </td><td> Fulmarus glacialoides </td></tr> <tr><td>Sooty Shearwater </td><td>sosh </td><td> Puffinus griseus </td></tr> <tr><td>South Polar Skua </td><td>spsk </td><td> Catharacta maccormicki </td></tr> <tr><td>Unknown Albatross </td><td>unal </td><td> nd </td></tr> <tr><td>Unidentified Petrel </td><td>unpe </td><td> nd </td></tr> <tr><td>Unidentified Prion </td><td>unpr </td><td> nd </td></tr> <tr><td>Unidentified Seal </td><td>unse </td><td> nd </td></tr> <tr><td>unidentified large Skua </td><td>unsk </td><td> nd </td></tr> <tr><td>Unidentified storm-petrel </td><td>unsp </td><td> nd </td></tr> <tr><td>Unidentified Whale </td><td>unwh </td><td> nd </td></tr> <tr><td>Weddell Seal </td><td>wese </td><td> Leptonychotes weddellii </td></tr> <tr><td>Wilsons Storm-petrel </td><td>wisp </td><td> Oceanites oceanicus </td></tr> </table><p> <table border cellspacing=0 cellpadding=5> <caption><b>Behavior Codes</b></caption> <tr><th>Code</th><th>Description</th><th>Explanation</th></tr> <tr><td> 1</td> <td>Feeding</td><td>Birds or seals observed handling foods or birds attempting to catch food</td></tr> <tr><td> 2</td> <td>Milling</td><td> Birds observed foraging or circling</td></tr> <tr><td> 3</td> <td>In transit</td><td>Birds or seals moving in a direct line in a definite direction</td></tr> <tr><td> 4</td> <td>Resting on Ice</td><td>Applies to both birds and seals </td></tr> <tr><td> 5</td> <td>Resting on Water</td><td>Applies to both birds and seals</td></tr> <tr><td> 6</td> <td>Following Ship</td><td> Birds only</td></tr> <tr><td> 7</td> <td>dipping, possible feeding</td> <td> </td></tr> <tr><td> 8</td> <td>Attracted to ship</td><td> </td> </tr> </table> <p> <table border cellspacing=0 cellpadding=5> <caption><b>Transect Codes</b></caption> <tr><th>Code</th><th>Description</th></tr> <tr><td> 3</td> <td>300 m transect on the port side</td></tr> <tr><td> 6</td> <td>600 m transect on the port side</td></tr> <tr><td> 0</td> <td>>600 m on port side</td></tr> <tr><td> 1</td> <td>Starboard side (No distance limit)</td></tr> </table> </p><p> <i>Last updated November 23, 2005; gfh</i> </pre> Seabird abundance and distribution within the SO GLOBEC study area was investigated using daytime and nighttime (using night vision viewers) survey work. We also recorded seal observations made within the transect area. Nighttime surveys were designed to complement daytime surveys. <ul> <li>Seabird Daytime Surveys<br> Strip transects were conducted simultaneously at 300 m and 600 m widths for birds. Surveys were conducted continuously while the ship was underway within the study area and when visibility was >300 m. For strip transects, two observers continuously scanned a 90Ôؽ area extending the transect distance (300 m and 600 m) to the side and forward along the transect line. Binoculars of 10X and 7X magnification were used to confirm species identifications. The 7X pair of binoculars also included a laser range finder. Ship followers and bird observed to be attracted to the ship were noted at first occurrence. These observations will be down-weighted in the analyses because these individuals may have been attracted to the ship from habitats at a distance from the ship. For each sighting, transect (300 m or 600 m), species, number of birds, behavior, flight direction, and any association with visible physical features, such as ice, were recorded. Distances were measured either by a range finder device as suggested by Heinemann (1981) or by the laser distance finder (when in the ice). Marine mammal sightings within the transect were also recorded. <p> Surveys were conducted from an outside observation post located on the port bridge wing of the RVIB N.B. Palmer. When it was not feasible to conduct surveys from this observation post, we surveyed from the inside port bridge wing. <li>Seabird Nighttime Surveys<br> ITT 200/210 Binocular Night Vision Viewers were used during one half-hour survey periods while on the survey grid. Surveys were a minimum of an hour apart. Observations were made from the bridge wing during NBP0104 and outside, from a dark area on the 01 deck, during NBP0103. Observers scanned back and forth looking for birds. Species and behavior of the bird was recorded for each observation. Observations were not conducted when visibility with the night vision viewer was less than 100 m from the ship. </UL> 10070 BMP2_ess BMP2_ess http://globec.whoi.edu/jg/serv/globec/soglobec/BMP2_ess.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/BMP2_ess%7D <h3 align=center> Environmental Data Stream (CTD Plus)<br> A Component of the BIOMAPERII Data Acquisition System</h3> <p> These data are from the Environmental Sensing System (ESS) a component of the <u>BIO </u>-Optical <u>M</u>ulti-frequency <u>A</u>coustical and <u>P</u>hysical <u>E</u>nvironmental <u>R</u>ecorder (BIOMAPER II)¹ data acquisition system.</p> <p> BIOMAPERII is a towed package consisting of a number of independent observational components: a multi-frequency sonar (Acoustics) system, a video plankton recorder (VPR) system, and an environmental sensor system (ESS). The incoming ESS environmental data is split into two data streams, one to be merged with the VPR data and one to be merged with the acoustics data. The reason being that there are times when either the Acoustic or VPR system may be turned off. Thus, there is a independent ESS data set to support either the Acoustic or VPR data streams. </p> <p> The ESS data reported here are in support of the Acoustics data stream. See the data object "sv120data", 120 kHz acoustic backscatter data set. <p> <h2>References</h2> &sup1;Wiebe, P.H., et al., 2002, BIOMAPER-II: An Integrated Instrument Platform for Coupled Biological and Physical Measurements in Coastal and Oceanic Regimes. IEEE Journal of Oceanic Engineering, <b>27(3)</b>:700-716.</p> <p>&sup2;Fofonoff and Millard, 1983, UNESCO technical papers in Marine Sciences, #44</p> <p> <b>Questions concerning this data set should be directed to:</b><br> Peter Wiebe<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543 <br> voice: (508) 289-2313 <br> fax: (508) 457-2169 <br> <a href="mailto:pwiebe@whoi.edu"> e-mail: pwiebe@whoi.edu</a><br> <p> <i>Last updated: Apr 20, 2006</i> </p> </pre> These data are from the Environmental Sensing System (ESS) a component of the BIO -Optical Multi-frequency Acoustical and Physical Environmental Recorder (BIOMAPER II)1 data acquisition system. 10071 biomaperII biomaperII http://globec.whoi.edu/jg/serv/globec/soglobec/biomaperII.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/biomaperII%7D <h3 align=center>BiomaperII Environmental data coincident with VPR data </h3> <p> <p> These data are from the Environmental Sensing System (ESS) a component of the <u>BIO </u>-Optical <u>M</u>ulti-frequency <u>A</u>coustical and <u>P</u>hysical <u>E</u>nvironmental <u>R</u>ecorder (BIOMAPER II)¹ data acquisition system.</p> <p> BIOMAPERII is a towed package consisting of a number of independent observational components: a multi-frequency sonar (Acoustics) system, a video plankton recorder (VPR) system, and an environmental sensor system (ESS). The incoming ESS environmental data is split into two data streams, one to be merged with the VPR data and one to be merged with the Acoustics data. There are times when either the Acoustic or VPR systems may be turned off. Thus, there is a independent ESS data set to support the Acoustic or VPR data streams. </p> <p> These are the ESS environmental data from the VPR data stream.</p> <p> &sup1;Wiebe, P.H., et al., 2002, BIOMAPER-II: An Integrated Instrument Platform for Coupled Biological and Physical Measurements in Coastal and Oceanic Regimes. IEEE Journal of Oceanic Engineering, <b>27(3)</b>:700-716.</p> <p>These data are preliminary. Large outliers in the data have been removed. No comparison has been made with the data reported from the vertical CTD or water bottle stations. The depth data are very noisy because the instrument was sending out lots of spurious information and there has been no attempt to smooth it.</p> <p> <b>Any questions, contact:</b><br> Carin Ashjian, Associate Scientist<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543 <br> voice: (508) 289-3457 <br> fax: (508) 457-2169 <br> e-mail: <a href="mailto:cashjian@whoi.edu">cashjian@whoi.edu</a><br> <br> <i>last updated April 20, 2006 </i> </p></pre> These data are from the Environmental Sensing System (ESS) a component of the BIO -Optical Multi-frequency Acoustical and Physical Environmental Recorder (BIOMAPER II)1 data acquisition system. <p> BIOMAPERII is a towed package consisting of a number of independent observational components: a multi-frequency sonar (Acoustics) system, a video plankton recorder (VPR) system, and an environmental sensor system (ESS). The incoming ESS environmental data is split into two data streams, one to be merged with the VPR data and one to be merged with the Acoustics data. There are times when either the Acoustic or VPR systems may be turned off. Thus, there is a independent ESS data set to support the Acoustic or VPR data streams. </p> <p>These data are preliminary. Large outliers in the data have been removed. No comparison has been made with the data reported from the vertical CTD or water bottle stations. The depth data are very noisy because the instrument was sending out lots of spurious information and there has been no attempt to smooth it.</p> 10072 chloro_vernet chloro_vernet http://globec.whoi.edu/jg/serv/globec/soglobec/fullchloro.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/chloro_vernet%7D <h2 align=center> Chlorophyll <i>a</i> and Phaeo Pigments from Bottle Casts <br> and Ice / Ice Cores </h2> <p><b> A short note on the "Southern Ocean Grid System":</b> The grid is a Cartesian plane covering the sample region in which distances are easy to calculate. The grid system used for SOGLOBEC is a universal transverse mercator (UTM) projection with a certain base point and rotation. The base point was chosen in the far south and the rotation was chosen to create one axis along the peninsula, and the other offshore. The units of UTM are meters, but the points are chosen in km rounded to the nearest km. Negative numbers mean that samples were taken southwest of the y axis or southeast of the x axis. For more details see: <a href="http://globec.whoi.edu/so-dir/soglobec.grid.txt"> Complete explanation of the Southern Ocean grid system. </a><p> <b>METHODS:</b><br>Chlorophylls were dissolved in 90% acetone and measured using a Turner Designs Digital 10-AU-05 Fluorometer. The instrument was calibrated using chlorophyll <i>a</i> standards from Sigma Chemicals as noted below.</p> <p align=left> <b>Calibration Notes: NBP0103</b><br> Calibrated at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: <dir> High Fd: 0.109 High tau: 1.970<br> Med Fd: 0.111 Med tau: 1.950<br> Low Fd: 0.109 Low tau: 2.215<br> </dir> <p align=left> <b>Calibration Notes: NBP0104</b><br> Calibrated at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: <dir> High Fd: 0.090 High tau: 1.982<br> Med Fd: 0.092 Med tau: 1.981<br> Low Fd: 0.100 Low tau: 2.215<br> </dir> </p> <p align=left> <b>Calibration Notes: NBP0202</b><br> Calibrated at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: <dir> High Fd: 0.109 High tau: 1.954<br> Med Fd: 0.103 Med tau: 1.949<br> Low Fd: 0.100 Low tau: 1.954<br> </dir> </p> <p align=left> <b>Calibration Notes: NBP0204</b><br> Calibrated at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: <dir> High Fd: 0.149 High tau: 1.887<br> Med Fd: 0.141 Med tau: 1.968<br> Low Fd: 0.149 Low tau: 1.938<br> </dir> </p> <br> <b>Data submitted by:</b> <p>Maria Vernet <br> Scripps Institute of Oceanography<br> University of California, San Diego<br> La Jolla, California 92093-0218<br> <br> Phone: 1-858-534-5322<br> email: <a href="mailto=mvernet@ucsd.edu">mvernet@ucsd.edu</a> </p> <p> <i>Last update: November 30, 2005; gfh</i></pre> Chlorophylls were dissolved in 90% acetone and measured using a Turner Designs Digital 10-AU-05 Fluorometer. <p align="left"> <b>Calibration Notes: NBP0204</b><br> Calibrated at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: </p><dir> High Fd: 0.149 High tau: 1.887<br> Med Fd: 0.141 Med tau: 1.968<br> Low Fd: 0.149 Low tau: 1.938<br> </dir> 10073 chloro_daly chloro_daly http://globec.whoi.edu/jg/serv/globec/soglobec/fullchlorodaly.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/chloro_daly%7D <h3 align=center>Chloro and Phaeo Pigments from CTD Bottle Casts<br>LMG0203 </h3> <p> <b>Instrument Notes:</b><br> Palmer Station's Fluorometer specs: Turner Fluorometer LE40603, <dir> MC#0007288<br> S/N = 5147<br> NSF#018695<br> </dir> <p align=left> <b>Calibration Notes: </b><br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: <dir> High Fd: 0.145 High tau: 2.301<br> Med Fd: 0.143 Med tau: 2.317<br> Low Fd: 0.145 Low tau: 2.501<br> </dir> <hr><p> <b>Data Contributed by:</b><br> Kendra Daly<br> College of Marine Science <br> University of South Florida <br> 140 Seventh Ave., South <br> St. Petersburg, FL 33701 <br><br> Phone: 727 553 1041 <br> E-mail: <a href ="mailto: kdaly@marine.usf.edu">kdaly@marine.usf.edu</a> <p> <p> <i> Last updated December 15, 2005; gfh </i> Chloro and Phaeo Pigments from CTD Bottle Casts LMG0203 <p align="left"> <b>Calibration Notes: </b><br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard.<br> Calibration values used were as follows: </p><dir> High Fd: 0.145 High tau: 2.301<br> Med Fd: 0.143 Med tau: 2.317<br> Low Fd: 0.145 Low tau: 2.501<br> </dir> 10074 uwchloro uwchloro http://globec.whoi.edu/jg/serv/globec/soglobec/uwchloro.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/uwchloro%7D <h2 align=center> Underway Chloro and Phaeo Pigments, <br> Hull Intake Sampling</h2> <p> <b> Methods: </b><br> Surface chlorophyll samples were collected from the ship's flow-through seawater system, which has seawater intakes between 5 and 7 meter depths on both ships. About one liter of seawater was vacuum filtered onto GF/F filters and passively extracted in 7 ml of 90% acetone at -20deg C in the dark for at least 24 hours. Chlorophyll fluorescence was then measured on a Turner Design Digital 10-AU-05 fluorometer calibrated prior to the cruise. </p> <p> <h3 align=center> Calibration Values </h3> <p><b>Southern Ocean GLOBEC II - Nathaniel B. Palmer 01-04</b></p> <p>Notes:<br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard. </p> <p>The following are the calibration values:<br> <table width=50% border=1> <tr align=center><th> &nbsp </th><th> Fd </th> <th> &nbsp </th> <th> tau </th> </tr> <tr> <td> H </td> <td> 0.109</td> <td> H </td> <td> 1.970 </td></tr> <tr> <td> M </td> <td>0.111 </td> <td>M </td> <td>1.950</td></tr> <tr> <td> L </td> <td> 0.109 </td> <td> L </td> <td> 1.928 </td> </tr> </table> </p> <hr> <p> <b>Southern Ocean GLOBEC III - Laurence M. Gould 02-03</b></p> <p>Notes:<br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard. </p> <p>The following are the calibration values:<br> <table width=50% border=1> <tr align=center><th> &nbsp </th><th> Fd </th> <th> &nbsp </th> <th> tau </th> </tr> <tr> <td> H </td> <td> 0.145</td> <td> H </td> <td> 2.301 </td></tr> <tr> <td> M </td> <td>0.143 </td> <td>M </td> <td>2.317</td></tr> <tr> <td> L </td> <td> 0.145 </td> <td> L </td> <td> 2.501 </td> </tr> </table> </p> <p><u>Study area</u>: <br> <b> Mean: </b> &nbsp &nbsp 1.15 <br> <b> SD</b>: &nbsp &nbsp 0.49 <br> <b> Median</b>: &nbsp &nbsp 1.10 <br> <b> Range</b>: &nbsp &nbsp 0.062-2.40 </p> <hr> <p> <b>Southern Ocean GLOBEC IV - Nathaniel B. Palmer 02-04</b></p> <p>Turner Designs 10-AU Fluorometer</p> <p>Notes:<br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard. </p> <p>The following are the calibration values: <br> <table width=50% border=1> <tr align=center><th> &nbsp </th><th> Fd </th> <th> &nbsp </th> <th> tau </th> </tr> <tr> <td> H </td> <td> 0.089</td> <td> H </td> <td> 2.276 </td></tr> <tr> <td> M </td> <td>0.086 </td> <td>M </td> <td>2.270</td></tr> <tr> <td> L </td> <td> 0.090 </td> <td> L </td> <td> 2.384 </td> </tr> </table> </p> <hr><br> <p> <b> Data Contributed by: </b><br> Kendra Daly<br> College of Marine Science<br> University of South Florida<br> 140 Seventh Ave., South <br> St. Petersburg, FL 33701 <br><br> Phone: 727 553 1041 <br> E-mail: <a href="mailto:kdaly@marine.usf.edu">kdaly@marine,usf.edu</a><br><br> <i>Last updated: December 16, 2005; gfh</i> </pre> Surface chlorophyll samples were collected from the ship&#039;s flow-through seawater system, which has seawater intakes between 5 and 7 meter depths on both ships. About one liter of seawater was vacuum filtered onto GF/F filters and passively extracted in 7 ml of 90% acetone at -20deg C in the dark for at least 24 hours. Chlorophyll fluorescence was then measured on a Turner Design Digital 10-AU-05 fluorometer calibrated prior to the cruise. <p> <b>Southern Ocean GLOBEC III - Laurence M. Gould 02-03</b></p> <p>Notes:<br> Performed serial dilution calibration at start of cruise using Sigma Chemicals chl_a standard. </p> <p>The following are the calibration values:<br> </p><table border="1" width="50%"> <tbody><tr align="center"><th> &nbsp; </th><th> Fd </th> <th> &nbsp; </th> <th> tau </th> </tr> <tr> <td> H </td> <td> 0.145</td> <td> H </td> <td> 2.301 </td></tr> <tr> <td> M </td> <td>0.143 </td> <td>M </td> <td>2.317</td></tr> <tr> <td> L </td> <td> 0.145 </td> <td> L </td> <td> 2.501 </td> </tr> </tbody></table> <p><u>Study area</u>: <br> <b> Mean: </b> &nbsp; &nbsp; 1.15 <br> <b> SD</b>: &nbsp; &nbsp; 0.49 <br> <b> Median</b>: &nbsp; &nbsp; 1.10 <br> <b> Range</b>: &nbsp; &nbsp; 0.062-2.40 </p> 10075 ctd_JK_one_meter ctd_JK_one_meter http://globec.whoi.edu/jg/serv/globec/soglobec/ctd_JK_one_meter.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ctd_JK_one_meter%7D <h2 align=center> CTD profile data from the Southern Ocean </h2> <p> <b>Note:</b><br> Some variables have been eliminated from the display but are nevertheless available. These variables include: Temperature0, Temperature1, Salinity0 and Salinity1. These variables are reported from the primary (0) and secondary (1) temperature and conductivity sensors. <br> <p align=left> John Klinck has provided <a href="http://www.mathworks.com">Matlab</a>^&#174; routines to use to read and display the data. When you use his routines you'll need to use the data in the format he provided or alter the routines to suit the data format you have. His routines are available in a package or individually. </p> <p> <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0103.event.tar.gz"> NBP0103.event.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0104.event.tar.gz"> NBP0104.event.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0202.event.tar.gz"> NBP0202.event.tar.gz</a>: <br> These have event files for all hydrographic events as well as separate files for ctd, xctd and xbt events. [<b>NB</b>: This data is also available directly <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/eventlogs.html0">on-line</a>]</p> <p><a href="http://globec.whoi.edu/globec-dir/CTD/NBP0103.ctd.tar.gz"> NBP0103.ctd.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0104.ctd.tar.gz"> NBP0104.ctd.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0202.ctd.tar.gz"> NBP0202.ctd.tar.gz</a>: <br> These files have two subdirectories (OneMeter and StdDepth) with ascii files for casts with the resolution indicated by the directory name. The files are ctdxxx.dat where xxx is the cast number, with leading zeros if necessary. The data in these files is self describing. The readctd routine in the matlab package will read these files. The first line in the file tells how many data items in the file (all ctd files have identical structure). </p> <p><b>(Package)</b> <a href="http://globec.whoi.edu/globec-dir/CTD/soglobec.matlab.tar.gz"> soglobec.matlab.tar.gz</a>: <br> This file has 5 subdirectories (Ctd, General, Grid, Oceans, SeaWater) with a bunch of tools for plotting the above ctd data. It uses the oceans and seawater routines that are widely available (but copies are included). There is also a set of routines to convert between lat-lon and a universal transverse mercator mapping that we use for station location. There is a startup.m file in "Ctd" to point to General, Oceans and SeaWater. In "Ctd" is a subdirectory (matlab) with various routines. The routines in the main directory are drivers to make multiple figures. There is documentation of these routines in the files and in the folders.</p> <p><b>(Individual routines)</b> <a href="http://globec.whoi.edu/globec-dir/CTDSoftware">soglobec.matlab</a>. Hint: Read routines in "General" first, then go to "Ctd" for startup.m file. </p> <p> New Hint (6/13/03): There is a new SetupPlots.m file in the "General" m-files folder. "This file chooses stations from the four cruises for the various plots. Since there was so little data from the 0204 cruise, individual lines across the grid were not specified(they may be later). A subset of the stations were chosen that are the "official" casts at each station occupied." <i>J.Klinck</i> </p> <p> <b>Data and Software provided by:</b><br> John M. Klinck<br> Center for Coastal Physical Oceanography<br> Department of Ocean, Earth and Atmospheric Sciences<br> Crittenton Hall<br> Old Dominion University<br> Norfolk, Virginia 23529<br><br> phone: 757 683-6005, fax: 757 683-5550<br> email: <a href="mailto: klinck@ccpo.odu.edu">klinck@ccpo.odu.edu</a> </p> <br> <i>File updated 01/04/2006; gfh</i> </pre> Some variables have been eliminated from the display but are nevertheless available. These variables include: Temperature0, Temperature1, Salinity0 and Salinity1. These variables are reported from the primary (0) and secondary (1) temperature and conductivity sensors. 10076 ctd_JK_std_depth ctd_JK_std_depth http://globec.whoi.edu/jg/serv/globec/soglobec/ctd_JK_std_depth.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ctd_JK_std_depth%7D <h2 align=center> CTD profile data from the Southern Ocean </h2> <p> <b>Note:</b><br> Some variables have been eliminated from the display but are nevertheless available. These variables include: Temperature0, Temperature1, Salinity0 and Salinity1. These variables are reported from the primary (0) and secondary (1) temperature and conductivity sensors. <br> <p align=left> John Klinck has provided <a href="http://www.mathworks.com">Matlab</a>^&#174; routines to use to read and display the data. When you use his routines you'll need to use the data in the format he provided or alter the routines to suit the data format you have. His routines are available in a package or individually. </p> <p> <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0103.event.tar.gz"> NBP0103.event.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0104.event.tar.gz"> NBP0104.event.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0202.event.tar.gz"> NBP0202.event.tar.gz</a>: <br> These have event files for all hydrographic events as well as separate files for ctd, xctd and xbt events. [<b>NB</b>: This data is also available directly <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/eventlogs.html0">on-line</a>]</p> <p><a href="http://globec.whoi.edu/globec-dir/CTD/NBP0103.ctd.tar.gz"> NBP0103.ctd.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0104.ctd.tar.gz"> NBP0104.ctd.tar.gz</a> and <a href="http://globec.whoi.edu/globec-dir/CTD/NBP0202.ctd.tar.gz"> NBP0202.ctd.tar.gz</a>: <br> These files have two subdirectories (OneMeter and StdDepth) with ascii files for casts with the resolution indicated by the directory name. The files are ctdxxx.dat where xxx is the cast number, with leading zeros if necessary. The data in these files is self describing. The readctd routine in the matlab package will read these files. The first line in the file tells how many data items in the file (all ctd files have identical structure). </p> <p><b>(Package)</b> <a href="http://globec.whoi.edu/globec-dir/CTD/soglobec.matlab.tar.gz"> soglobec.matlab.tar.gz</a>: <br> This file has 5 subdirectories (Ctd, General, Grid, Oceans, SeaWater) with a bunch of tools for plotting the above ctd data. It uses the oceans and seawater routines that are widely available (but copies are included). There is also a set of routines to convert between lat-lon and a universal transverse mercator mapping that we use for station location. There is a startup.m file in "Ctd" to point to General, Oceans and SeaWater. In "Ctd" is a subdirectory (matlab) with various routines. The routines in the main directory are drivers to make multiple figures. There is documentation of these routines in the files and in the folders.</p> <p><b>(Individual routines)</b> <a href="http://globec.whoi.edu/globec-dir/CTDSoftware">soglobec.matlab</a>. Hint: Read routines in "General" first, then go to "Ctd" for startup.m file. </p> <p> New Hint (6/13/03): There is a new SetupPlots.m file in the "General" m-files folder. "This file chooses stations from the four cruises for the various plots. Since there was so little data from the 0204 cruise, individual lines across the grid were not specified(they may be later). A subset of the stations were chosen that are the "official" casts at each station occupied." <i>J.Klinck</i> </p> <p> <b>Data and Software provided by:</b><br> John M. Klinck<br> Center for Coastal Physical Oceanography<br> Department of Ocean, Earth and Atmospheric Sciences<br> Crittenton Hall<br> Old Dominion University<br> Norfolk, Virginia 23529<br><br> phone: 757 683-6005, fax: 757 683-5550<br> email: <a href="mailto: klinck@ccpo.odu.edu">klinck@ccpo.odu.edu</a> </p> <br> <i>File updated 01/04/2006; gfh</i> </pre> CTD profile data from the Southern Ocean. Some variables have been eliminated from the display but are nevertheless available. These variables include: Temperature0, Temperature1, Salinity0 and Salinity1. These variables are reported from the primary (0) and secondary (1) temperature and conductivity sensors. 10077 ctd_cruise ctd_cruise http://globec.whoi.edu/jg/serv/globec/soglobec/ctd_cruise.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ctd_cruise%7D <h3 align=center>Sea-Bird CTD Data Files</h3> <p>These CTD data files were collected on most cruises. The raw and processed data were placed on CD-ROMs, usually in zipped and/or tar'ed form, and provided to the participants and the Data Management Office. The "asc" versions of the files are served, using the information collected from the "hdr" files. These files have been shipboard processed using standard SeaBird software to one decibar averaged intervals.</p> <p>If a cruise is not represented here, there were no ascii files available to serve (lmg0103, lmg0104, lmg0106). </p> <p> <b>Questions concerning this data set should be directed to:</b><br> Bob Groman <br> Globec Data Management Office <br> Woods Hole Oceanographic Institution <br> Woods Hole, MA 02543 <br> Phone: 508 289 2409<br> E-mail: rgroman@whoi.edu<br><br> <i>Last updated February 24, 2006</i><pre> </pre> Sea-Bird CTD Data Files. These files have been shipboard processed using standard SeaBird software to one decibar averaged intervals. 10078 daily_PAR daily_PAR http://globec.whoi.edu/jg/serv/globec/soglobec/allpar_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/daily_PAR%7D? <h3 align=center> Photosynthetically Available Radiation (PAR) Data <br> from broadscale cruises NBP0103, NBP0104, NBP0202 and NBP0204</h3> <p> <b>Instrument Notes:</b> <br> Biospherical Instruments GUV-500 is a 5-channel reference radiometer which typically measures cosine-corrected down welling irradiance at 305, 320, 340, 380nm and PAR (400-700nm). Cosine irradiance (EsPAR) sensors collect light impinging on a Teflon-coated diffuser and the response is proportional to the cosine of the angle of incidence.<br><p> Biospherical Instruments QSR250 system measures a single channel of scalar irradiance (PAR) and is appropriate for applications independent of the directionality of the light field, such as measurements of the flux available for photosynthesis.<br> <i> -- Biospherical Instruments </i> </p> <p> <b> Data Notes: </b><br> 1. The cosine PAR value for yrday_gmt 151 year 2001 is an estimate, based on a conversion from data recorded by the QSR240 scalar sensor package.<br> 2. Latitude and longitude have been added to this data set by the Data Management Office. These positions are the noon (12:00 hour) positions reported in the ship's alongtrack data set. <br> 3. Scalar PAR data was extracted from the ship's alongtrack meteorological data set. The sensor package was mounted on ship's science mast.</p> <p> <b>Methods:</b><br> For additional information on methods see the on-line cruise reports, (Primary Production Sections) <a href="http://globec.whoi.edu/so-dir/reports/nbp0103/nbp0103.html">nbp0103</a>, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory%7D?project%20eq%20NBP0104,data_type%20eq%20cruise_report">nbp0104 </a>, <a href="http://globec.whoi.edu/so-dir/reports/nbp0202/nbp0202b.html#TOC1_6">nbp0202</a>, and <a href="http://globec.whoi.edu/so-dir/reports/nbp0204/nbp0204b.html#TOC1_8">nbp0204</a>. </p> <p> <b>Data contributed by:</b><br> Maria Vernet<br> Integrative Oceanographic Division<br> Scripps Institution of Oceanography<br> University of California San Diego<br> La Jolla, California 92093-0218</p> <p>Phone: 1-858-534-5322<br> E-mail: <a href="mailto:mvernet@ucsd.edu">mvernet@ucsd.edu</a></p> <p><i>Last updated: December 09, 2005; gfh</i></p> </pre> <ul><li>The cosine PAR value for yrday_gmt 151 year 2001 is an estimate, based on a conversion from data recorded by the QSR240 scalar sensor package. <li>Latitude and longitude have been added to this data set by the Data Management Office. These positions are the noon (12:00 hour) positions reported in the ship&#039;s alongtrack data set. <li>Scalar PAR data was extracted from the ship&#039;s alongtrack meteorological data set. The sensor package was mounted on ship&#039;s science mast. </ul> For additional information on methods see the on-line cruise reports, (Primary Production Sections) <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory%7D?project%20eq%20NBP0104,data_type%20eq%20cruise_report">nbp0104 </a>. 10079 DIF_records DIF_records http://globec.whoi.edu/jg/serv/globec/soglobec/dif_records.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/DIF_records%7D <h3 align=center> DIF records </h3> <p>Metadata has been submitted to the <a href="http://nsidc.org/usadcc/">U.S. Antarctic Data Coordination Center</a> as part of the grantee obligation.</p> <p>In general, any metadata record can be accessed directly through the URL:<br> http://gcmd.nasa.gov/getdif.htm?[entry_id]</p> where [entry_id] = the Entry_ID of the metadata record, e.g. simrad_SO</p> 10080 drifter_images drifter_images http://globec.whoi.edu/jg/serv/globec/soglobec/drifters.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/drifter_images%7D <pre> <b>PI:</b> R.Limeburner <b>dataset:</b> Drifter tracks Parameter Description Units <hr> images Image name n/a movie Movie name n/a, fli format description Description of data n/a file_date Date of image file monthday </pre> <p>Note, for the "flc" animations you will need a movie player capable of reading *.fli/*.flc type movies. The <a href="http://usjgofs.whoi.edu/globec-dir/aaplay.html">Autodesk Animation Player</a> is one such player. </pre> 10081 drifters_argos drifters_argos http://globec.whoi.edu/jg/serv/globec/soglobec/drifters_argos.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/drifters_argos%7D <h2 align=center>ARGOS Tracked Near Surface Drifter Data</h2> <p> The following was extracted from the Cruise Report of the N.B. Palmer Cruise 01-03. The complete cruise report can be see on the SO GLOBEC web site under the object "Inventory"<br><br> 2.0 Drifter Measurements (Bob Beardsley and Dick Limeburner)<br><br> Surface drifters are being deployed and tracked via satellite to study the near surface Lagrangian currents in the SO GLOBEC study area on the western Antarctic Peninsula Shelf. Each drifter has a small (~ 30 cm diameter) surface float with ARGOS transmitter and batteries tethered to a holey sock drogue centered at 15 m below the surface. The drogue, about 10 m tall and 1 m in diameter, is designed to "lock" itself to the water so that the surface float follows the mean water motion at 15 m depth with very little slippage even in high winds. Thus measuring the drifter's position as a function of time provides a Lagrangian measurement of the 15-m ocean current.<br><br><br> <b>Data contributed by:</b><br> Richard Limeburner<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br><br> e-mail: <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a><br><br><br> <i>file updated January 5, 2006, gfh</i> 2.0 Drifter Measurements (Bob Beardsley and Dick Limeburner)<br><br> Surface drifters are being deployed and tracked via satellite to study the near surface Lagrangian currents in the SO GLOBEC study area on the western Antarctic Peninsula Shelf. Each drifter has a small (~ 30 cm diameter) surface float with ARGOS transmitter and batteries tethered to a holey sock drogue centered at 15 m below the surface. The drogue, about 10 m tall and 1 m in diameter, is designed to "lock" itself to the water so that the surface float follows the mean water motion at 15 m depth with very little slippage even in high winds. Thus measuring the drifter&#039;s position as a function of time provides a Lagrangian measurement of the 15-m ocean current. 10082 krill krill http://globec.whoi.edu/jg/serv/globec/soglobec/krill.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/krill%7D <h3 align=center>Euphausiid Abundance, Based on Life Stage and Size<br> Collected during the Process Cruises, Austral Autumn 2001 and 2002</h3> <p><b>Data Contributed By:</b><br> Kendra L. Daly <br> College of Marine Science<br> University of South Florida<br> 140 Seventh Ave. S.<br> St. Petersburg, FL 33701<br> <br> Phone: 727-553-1041<br> E-Mail: <a href= "mailto: kdaly@marine.usf.edu">kdaly@marine.usf.edu</a> </p> <p>Net sample collections: Meng Zhou, Yiwu Zhu, Ryan Dorland, Dan Mertes, and Joe Smith </p> <p>Sample Analyses: Jason Zimmerman, Alexander Timonin, Tatjana Semenova</p> <p>Cruises:<br /> <span class="style2"><i>Laurence M. Gould</i>, 23 April - 6 June 2001 (<a href="http://www.ccpo.odu.edu/Research/globec/cruises01/nbp0104_menu.html">LMG0104 cruise report</a>), 18 net tows<br /> <i>Laurence M Gould</i>, 7 April - 21 May 2002 (<a href="http://www.ccpo.odu.edu/Research/globec/main_cruises02/lmg0203/menu.html">LMG0203 cruise report</a>), 16 net tows</span></p> <p><b>Methods</b> </p> <p>Zooplankton abundance, vertical and horizontal distribution, and population structure were assessed using a 1 m² Multiple Opening and Closing Nets and Environmental Sampling System (MOCNESS) with nine nets having 333 ¬µm mesh and environmental sensors of temperature, salinity and depth. The entire water column was sampled on the downcast using net # 0, which was not analyzed. The upper water column was typically sampled using nets 1 and 2 from 500 m to 200 m at 150 m depth intervals, nets 3 and 4 from 200 m to 100 m at 50 m depth intervals, and nets 5 to 8 from 100 m to the surface at 25 m depth intervals. Some tows were deployed down to 1000 m, and some tows were towed targeting krill swarms at irregular depths. Approximate locations of process study stations are shown in <a href="#Figure1">Fig. 1</a>. More precise locations of the casts in <a href="#fig2">Fig. 2</a>.</p> <p>Zooplankton samples were immediately preserved in 10% buffered formalin solution. All the large organisms (>15 mm) in the sample were removed and identified to taxa. The sample was then split to about 100 individuals of euphausiids. All euphausiids in the split were identified to species and life history stage and measured for length to the nearest 0.5 mm for larvae and to the nearest 1.0 mm for juvenile and adults. Next the sample was split to about 100 individuals of copepods. Copepods were identified to species and life history stage (female, male, copepodite V, or other copepodite). All other zooplankton in the split were identified to taxa and counted. For the Euchaetidae, we followed the designation of Park (1994) who ascribed the Antarctic species to the genus <i>Paraeuchaeta</i>. This data object ("krill") reports the abundance of each euphausiid species by life stage and size class. The companion data object "zooabund" reports the counts of zooplankton per subsample/split by taxa and life stage or size class. </p> <p><a href="kdaly_PI_notes.html">More methodology notes.</a></p> <p>Greenwich Mean Time was local time + 4 hours.</p> <p>Reference:</p> <blockquote> <p>Park, T. 1994. Taxonomy and distribution of the marine calanoid copepod family Euchaetidae. Bulletin of the Scripps Institution of Oceanography University of California, San Diego v. 29, University of California Press, Berkeley, CA, 203 pp. </p> </blockquote> <p align="center"><a name="Figure1" id="Figure1"></a><a href="http://globec.whoi.edu/images/image002kdaly.gif"><img width=581 height=464 src="http://globec.whoi.edu/images/image002kdaly.gif"></a></p> <p>Fig. 1. Approximate locations of process cruise stations in Marguerite Bay during austral autumn 2001 and 2002.</p> <p align="center"><a name="fig2" id="fig2"></a><a href="http://globec.whoi.edu/images/MOC_station_map_LMG.png"><img src="http://globec.whoi.edu/images/MOC_station_map_LMG.png" alt="MOCNESS station map" width="629" height="406" /></a></p> <p>Fig. 2. Locations of MOCNESS stations for LMGould-0104 (2001) and LMGould-0203 (2002) cruises. Numbers correspond to the cast number.</p> <p>Additional notes by PI.</p> <p><strong>Notes on Volume Filtered values:</strong></p> <p>The 1 m2 MOCNESS net volume filtered data were corrected for the following net tows:</p> <p>The flowmeter used to calculate the volume of water filtered <b>did not work</b> for the tows shown below; the data shown in the listings for those tows are therefore <b>derived, not measured</b>. Using the net distance and the average angle of the net, the volume filtered was estimated. These estimates have about a 10% error or higher when currents were present. </p> <p>2001: No further corrections. MOC-1 net volume filtered values were used to calculate abundance/m3 for all net tows. No Optical Plankton Counter (OPC) volume filtered values were available for 2001.</p> <p>2002: The flowmeter data was not accurate for some net tows in 2002. Optical Plankton Counter (OPC) volume filtered was used to calculate abundance/m3 for all MOC-1 net tows, except casts 11 and 16 which used the MOC-1 volume filtered values. The decision to use OPC values was determined by plotting all OPC volume filtered numbers versus MOC-1 flow meter data (see below). MOC-1 flow meter data were consistently lower and had a lower R2 regression for volume filtered versus length of tow (time). Meng Zhou and Yiwi Zhu, who conducted the MOC-1 net tows, noted on the haul sheets that there were problems with the MOC-1 flow meters and that they often were not responsive or worked intermittently. Thus, it was decided that the OPC flow meter data provided a more consistent measure of net flow volume for 2002 net tows. The OPC mouth opening for flow meter data was corrected to the MOC-1 net mouth opening by multiplying the OPC flow data by 200. The two casts that used MOC-1 flow meter data were cases where the OPC flow meter data appeared to underestimate the flow.</p> <p align="center"><a href="http://globec.whoi.edu/images/kdaly_volfilt_info4.png"><img src="http://globec.whoi.edu/images/kdaly_volfilt_info4.png" alt="LMG0202 volume filtered: MOC and OPC" width="586" height="384" /></a> </p> <p align="center">Fig. 3. Volume filtered over time for both MOCNESS and Optical Plankton Counter showing consistently lower flow rates for the MOCNESS.</p> <p><strong>DMO Note:</strong> </p> <p>Revised data received Jan. 2008. Reformatted for this data system from Excel spreadsheets, joined with event log metadata (date, lat, lon, depth_w) using 8200 server and restructured using rs 2.0 before serving here. Each individual euphausiid is listed with its length. The abundance for each length bin is given beside the last specimen for that bin. The abundance for the stage and species are shown beside the last specimen of each stage and species, respectively. <a href="kdaly_dmo-notes.html">Changes and further notes</a> -- njc 7/7/08</p> <p><i><span class="style1"><em>updated January 6, 2006, gfh</em><br /> updated July 30, 2008, njc</span></i> </p> 10083 eventlogs eventlogs http://globec.whoi.edu/jg/serv/globec/soglobec/eventlogs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/eventlogs%7D Event logs provide an overall summary of the sampling activities during a cruise. A hard copy of the event log is also included in each cruise report. <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a><p> <p> <i>Last updated July 05, 2007; mda</i> 10084 inventory inventory http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory%7D <h2 align=center>Inventory of U.S. GLOBEC Southern Ocean Data</h2> This inventory uses the JGOFS data management system and the same hierachical data structure used in many other data sets to store data about the data (metadata). Data fields include: <p> For further information contact the <a href="http://globec.whoi.edu/globec-dir/contact_dmo.html">Data Management Office</a> 10085 mean_rates mean_rates http://globec.whoi.edu/jg/serv/globec/soglobec/mean_rates_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/mean_rates%7D <h3 align=center>Mean respiration and excretion rates for micronekton<br> Southern Ocean GLOBEC</h3> <p> </p> <p> <b>Collection of specimens.</b> Crustaceans were collected using either mouth-closing Tucker trawls (9.0 m² or 2.25 m² mouth area) or downward-looking, vertically deployed plummet nets (1 m² mouth area). Tucker trawls were equipped with either blind or thermal-turbulence-protecting cod-ends (Childress et al. 1978); plummet nets terminated in bind cod-ends only. Specimens were taken in the upper 1000m of the water column in the vicinity of the marginal ice zone during spring (November-December) 1983, fall (March) 1986, and winter (June-August) 1988 as part of the AMERIEZ (Antarctic Marine Ecosystem Research at the Ice Edge Zone) program to study ice edge biology. Sampling locations were all in the Scotia-Weddell Sea region but moved with seasonal movement of the pack ice edge. Thus, spring and winter collections were in the Scotia Sea in the vicinity of 60deg S, 40deg W; fall sampling took place further south, 65deg S, 46deg W. Collections were made on a continuum from deep in the pack ice out to 300 km seaward of the ice edge in fall and winter. In spring, collections were made in the open water only. Station locations are given in Donnelly <i>et al.</i> (1990). <p>Oxygen consumption rates were determined by allowing individuals to deplete the oxygen in a sealed container filled with filtered (0.45 um pore size) seawater. Temperature was maintained at 0.5 C (+/- 0.1 C) using a refrigerated water bath. Oxygen partial pressure (PO₂) was continuously monitored using a Clark polarographic oxygen electrode (Clark 1956) as an individual reduced oxygen levels to low (10 to 20 mm Hg) partial pressures. Electrodes were calibrated using air- and nitrogen-saturated seawater at the experimental temperature. The time required for consumption of oxygen to low levels varied from 12 to 18 h. Streptomycin and Neomycin (each 25 mg 1^-1) were added to the seawater to minimize microbial growth. To control for possible oxygen consumption by microorganishs, an individual was removed after selected runs, its volume was replaced with fresh seawater, and oxygen consumption was again measured for 2 to 4 h. In all cases microbial oxygen consumption was negligibly low.</p> <p>References:<br> Torres, Joseph J., <i>et al.</i>, 2007; The physiology of autumn and winter krill (<i>Euphausia superba</i>) in the waters of the Western Antarctic Peninsula Shelf. <i>GLOBEC International Newsletter</i>, <b>13</b>:1, 60-62.</p> <p> <b>Contact:</b><br> Jose Torres<br> College of Marine Science<br> University of South Florida<br> 140 Seventh Avenue, South<br> St. Petersburg, FL 33701<br> <a href="mailto:jtorres@marine.usf.edu">jtorres@marine.usf.edu</a> </p> <b>Collection of specimens.</b> Crustaceans were collected using either mouth-closing Tucker trawls (9.0 m² or 2.25 m² mouth area) or downward-looking, vertically deployed plummet nets (1 m² mouth area). Tucker trawls were equipped with either blind or thermal-turbulence-protecting cod-ends (Childress etal. 1978); plummet nets terminated in bind cod-ends only. Specimens were taken in the upper 1000m of the water column in the vicinity of the marginal ice zone during spring (November-December) 1983, fall (March) 1986, and winter (June-August) 1988 as part of the AMERIEZ (Antarctic Marine Ecosystem Research at the Ice Edge Zone) program to study ice edge biology. Sampling locations were all in the Scotia-Weddell Sea region but moved with seasonal movement of the pack ice edge. Thus, spring and winter collections were in the Scotia Sea in the vicinity of 60Ôؽ S, 40Ôؽ W; fall sampling took place further south, 65Ôؽ S, 46Ôؽ W. Collections were made on a continuum from deep in the pack ice out to 300 km seaward of the ice edge in fall and winter. In spring, collections were made in the open water only. Station locations are given in Donnelly etal (1990). Oxygen consumption rates were determined by allowing individuals to deplete the oxygen in a sealed container filled with filtered (0.45 um pore size) seawater. Temperature was maintained at 0.5 C (+/- 0.1 C) using a refrigerated water bath. Oxygen partial pressure (PO₂) was continuously monitored using a Clark polarographic oxygen electrode (Clark 1956) as an individual reduced oxygen levels to low (10 to 20 mm Hg) partial pressures. Electrodes were calibrated using air- and nitrogen-saturated seawater at the experimental temperature. The time required for consumption of oxygen to low levels varied from 12 to 18 h. Streptomycin and Neomycin (each 25 mg 1^-1) were added to the seawater to minimize microbial growth. To control for possible oxygen consumption by microorganishs, an individual was removed after selected runs, its volume was replaced with fresh seawater, and oxygen consumption was again measured for 2 to 4 h. In all cases microbial oxygen consumption was negligibly low. 10086 mean_rates_fish mean_rates_fish http://globec.whoi.edu/jg/serv/globec/soglobec/mean_rates_fish_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/mean_rates_fish%7D <h3 align=center>Mean respiration and excretion rates for fish<br> Southern Ocean GLOBEC</h3> <p> <b>Contact:</b><br> Jose Torres<br> College of Marine Science<br> University of South Florida<br> 140 Seventh Avenue, South<br> St. Petersburg, FL 33701<br> <a href="mailto:jtorres@marine.usf.edu">jtorres@marine.usf.edu</a> </p> <b>Collection of specimens.</b> Crustaceans were collected using either mouth-closing Tucker trawls (9.0 m² or 2.25 m² mouth area) or downward-looking, vertically deployed plummet nets (1 m² mouth area). Tucker trawls were equipped with either blind or thermal-turbulence-protecting cod-ends (Childress etal. 1978); plummet nets terminated in bind cod-ends only. Specimens were taken in the upper 1000m of the water column in the vicinity of the marginal ice zone during spring (November-December) 1983, fall (March) 1986, and winter (June-August) 1988 as part of the AMERIEZ (Antarctic Marine Ecosystem Research at the Ice Edge Zone) program to study ice edge biology. Sampling locations were all in the Scotia-Weddell Sea region but moved with seasonal movement of the pack ice edge. Thus, spring and winter collections were in the Scotia Sea in the vicinity of 60° S, 40° W; fall sampling took place further south, 65° S, 46° W. Collections were made on a continuum from deep in the pack ice out to 300 km seaward of the ice edge in fall and winter. In spring, collections were made in the open water only. Station locations are given in Donnelly etal (1990). Oxygen consumption rates were determined by allowing individuals to deplete the oxygen in a sealed container filled with filtered (0.45 um pore size) seawater. Temperature was maintained at 0.5°C (±0.1°C) using a refrigerated water bath. Oxygen partial pressure (PO₂) was continuously monitored using a Clark polarographic oxygen electrode (Clark 1956) as an individual reduced oxygen levels to low (10 to 20 mm Hg) partial pressures. Electrodes were calibrated using air- and nitrogen-saturated seawater at the experimental temperature. The time required for consumption of oxygen to low levels varied from 12 to 18 h. Streptomycin and Neomycin (each 25 mg 1^-1) were added to the seawater to minimize microbial growth. To control for possible oxygen consumption by microorganishs, an individual was removed after selected runs, its volume was replaced with fresh seawater, and oxygen consumption was again measured for 2 to 4 h. In all cases microbial oxygen consumption was negligibly low. 10087 mean_rates_plankton mean_rates_plankton http://globec.whoi.edu/jg/serv/globec/soglobec/mean_rates_plankton_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/mean_rates_plankton%7D <h3 align=center>Mean respiration and excretion rates for plankton<br> Southern Ocean GLOBEC</h3> <p> <b>Contact:</b><br> Jose Torres<br> College of Marine Science<br> University of South Florida<br> 140 Seventh Avenue, South<br> St. Petersburg, FL 33701<br> <a href="mailto:jtorres@marine.usf.edu">jtorres@marine.usf.edu</a> </p> <b>Collection of specimens.</b> Crustaceans were collected using either mouth-closing Tucker trawls (9.0 m² or 2.25 m² mouth area) or downward-looking, vertically deployed plummet nets (1 m² mouth area). Tucker trawls were equipped with either blind or thermal-turbulence-protecting cod-ends (Childress etal. 1978); plummet nets terminated in bind cod-ends only. Specimens were taken in the upper 1000m of the water column in the vicinity of the marginal ice zone during spring (November-December) 1983, fall (March) 1986, and winter (June-August) 1988 as part of the AMERIEZ (Antarctic Marine Ecosystem Research at the Ice Edge Zone) program to study ice edge biology. Sampling locations were all in the Scotia-Weddell Sea region but moved with seasonal movement of the pack ice edge. Thus, spring and winter collections were in the Scotia Sea in the vicinity of 60° S, 40° W; fall sampling took place further south, 65° S, 46° W. Collections were made on a continuum from deep in the pack ice out to 300 km seaward of the ice edge in fall and winter. In spring, collections were made in the open water only. Station locations are given in Donnelly etal (1990). Oxygen consumption rates were determined by allowing individuals to deplete the oxygen in a sealed container filled with filtered (0.45 um pore size) seawater. Temperature was maintained at 0.5°C (±0.1°C) using a refrigerated water bath. Oxygen partial pressure (PO₂) was continuously monitored using a Clark polarographic oxygen electrode (Clark 1956) as an individual reduced oxygen levels to low (10 to 20 mm Hg) partial pressures. Electrodes were calibrated using air- and nitrogen-saturated seawater at the experimental temperature. The time required for consumption of oxygen to low levels varied from 12 to 18 h. Streptomycin and Neomycin (each 25 mg 1^-1) were added to the seawater to minimize microbial growth. To control for possible oxygen consumption by microorganishs, an individual was removed after selected runs, its volume was replaced with fresh seawater, and oxygen consumption was again measured for 2 to 4 h. In all cases microbial oxygen consumption was negligibly low. 10088 mocness_biovols mocness_biovols http://globec.whoi.edu/jg/serv/globec/soglobec/mocness_biovols_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/mocness_biovols%7D? <h3 align=center> Southern Ocean Biovolume Data from the MOCNESS tows<br> during the Broadscale Cruises, Austral Autumn 2001 and 2002<br> NB Palmer </h3> <p>This data set is derived from <a href="http://globec.whoi.edu/globec-dir/data_doc/dvolmethod_globecweb.htm"> displacement volume measurements</a> and dry weight <a href="#methods"> conversion calculations</a>.&nbsp; The MOCNESS-1 plankton sampler has nine rectangular nets (1m x 1.4 m) with a mesh size of 0.333 mm, which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976).</p> <p><b>Cruises:</b><br> Nathaniel B. Palmer, April-June 2001 (NBP01-03), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0103,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, July-Sept. 2001 (NBP01-04), 17 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0104,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, April-May 2002 (NBP02-02), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0202,data_type%20eq%20cruise_report"> cruise report</a> <br> Nathaniel B. Palmer, July-Sept. 2002 (NBP02-04), 19 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0204,data_type%20eq%20cruise_report"> cruise report</a></p> <p><b><a name="methods"></a>Methods:</b><br> ^<b>1</b>Displacement volume measurement:<br> Entire sample plus liquid was measured in a large graduated cylinder then poured through a sieve into a second cylinder. The difference in volume is the displacement volume. Detailed instructions are available <a href="http://globec.whoi.edu/globec-dir/data_doc/dvolmethod_globecweb.htm">here</a>.</p> <p>^<b>2</b>Dry weight calculations:<br> dry weight = (dvol/(10^0.139))^(1/1.003); [mg/m³]<br> integrated dry weight = depth interval * dry weight; [mg/m²]<br> total dry weight for the entire sampled water column = sum of integrated dry weights for all nets for one tow; [mg/m²]</p> This displacement volume data comes from nets with a mesh size of 333 &micro;m.<br> <br> <b>See companion files:</b> &nbsp;<br> -&nbsp; <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/zoo_moc.html0{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/zoo_moc}">Zooplankton Biomass and Abundance from MOCNESS tows using silhouette analysis</a>: NB Palmer, austral fall &amp; winter of 2001 &amp; 2002.&nbsp; Biomass (wet weight) and abundance were determined principally by silhouette digitization of taxa lengths and conversion to equivalent wet weights according to the equations and methods adapted from Davis and Wiebe (1985) and Wiebe et al. (2004). <p> - <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/zooabund_nbp.html0{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/zooabund_nbp}"> Zooplankton Abundance Based on Taxa and Life Stages or Size</a> Collected during the Broadscale Cruises, Austral Autumn 2001 and 2002, NB Palmer.&nbsp; These abundance values on the same tows were derived by counting and identifying a subset of the zooplankton to the species and life stage for euphausiids and dominant copepods and to taxonomic group with broad size categories for other zooplankton (pteropod, chaetognath, polychaete, etc.). <p><b>References:</b> <p>Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. Journal of Marine Research, <b>34(3)</b>: 313-326.</p> <p><b>Contact:</b><br> Nancy Copley<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br>email: <a href="mailto:ncopley@whoi.edu">ncopley@whoi.edu</a></p> <p>last updated: 16 Aug. 2006 (njc)</p> <p>This data set is derived from <a href="http://globec.whoi.edu/globec-dir/data_doc/dvolmethod_globecweb.htm"> displacement volume measurements</a> and dry weight <a href="#methods"> conversion calculations</a>.&nbsp; The MOCNESS-1 plankton sampler has nine rectangular nets (1m x 1.4 m) with a mesh size of 0.333 mm, which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976).</p> ^<b>1</b>Displacement volume measurement:<br> Entire sample plus liquid was measured in a large graduated cylinder then poured through a sieve into a second cylinder. The difference in volume is the displacement volume. Detailed instructions are available <a href="http://globec.whoi.edu/globec-dir/data_doc/dvolmethod_globecweb.htm">here</a>.</p> <p>^<b>2</b>Dry weight calculations:<br> dry weight = (dvol/(10^0.139))^(1/1.003); [mg/m³]<br> integrated dry weight = depth interval * dry weight; [mg/m²]<br> total dry weight for the entire sampled water column = sum of integrated dry weights for all nets for one tow; [mg/m²]</p> This displacement volume data comes from nets with a mesh size of 333 µm. 10089 nutrients nutrients http://globec.whoi.edu/jg/serv/globec/soglobec/fullnuts.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/nutrients%7D <h2 align=center>Nutrients from Bottle Casts</h2> <p> <h3 align=center>Methods </h3> <p>Analytical methods used for silica, phosphate, nitrite, and nitrate follow the recommendations of Gordon et al. (1993) for the WOCE WHP project. </p> <p>The analytical system we employ is a five-channel Technicon Autoanalyzer II upgraded with new heating baths, proportional pumps, colorimeters, improved optics, and an analog to digital conversion system (New Analyzer Program v. 2.40 by Labtronics, Inc.) This Technicon is designed for shipboard as well as laboratory use. </p> <p>Silica is determined by forming the heteropoly acid of dissolved orthosilicic acid and ammonium molybdate, reducing it with stannous chloride, and then measuring its optical transmittance.</p> <p>Phosphate is determined by creating the phosphomolybdate heteropoly acid in much the same way as with the silica method. However, its reducing agent is dihydrazine sulfate, after which its transmittance is also measured. A heating bath is required to maximize the color yield. </p> <p>Nitrite is determined essentially by the Bendschneider and Robinson (1952) technique in which nitrite is reacted with sulfanilamide (SAN) to form a diazotized derivative that is then reacted with a substituted ethylenediamine compound (NED) to form a rose pink azo dye which is measured colorimetrically. </p> <p>Nitrate is determined by difference after a separate aliquot of a sample is passed through a Cd reduction column to convert its nitrate to nitrite, followed by the measurement of the "augmented" nitrite concentration using the same method as in the nitrite analysis. </p> <p>In the analytical ammonia method, ammonium reacts with alkaline phenol and hypochlorite to form indophenolblue. Sodium nitroferricyanide intensifies the blue color formed, which is then measured in a colorimeter of our nutrient-analyzer. Precipitation of calcium and magnesium hydroxides is eliminated by the addition of sodium citrate complexing reagent. A heating bath is required. Our version of this technique is based on modifications of published methods such as the article by F. Koroleff in Grasshoff (1976). These modifications were made at Alpkem (now Astoria-Pacific International, Inc.) and at L.Gordon's nutrient laboratory at Oregon State University.</p> <h3 align=center>Data</h3> <p>Nitrate, nitrite, phosphate, ammonia, and silica were measured from every niskin bottle tripped from all hydrocasts on this cruise. All concentrations are reported in micromoles per liter.</p> <p><b>References</b></p> <p>Gordon, L.I., J.C. Jennings, Jr., A.A. Ross, and J.M. Krest, A Suggested Protocol For Continuous Flow Automated Analysis of Seawater Nutrients, in WOCE Operation Manual, WHP Office Report 90-1, <b>WOCE Report 77 No. 68/91, 1-52, 1993.</b></p> <p>Grasshoff, K. 1976. <b>Methods of Seawater Analysis</b>, Verlag Chemie, Weinheim, Germany, and New York, NY, 317 pp.</p><br> <p> <b> Data Contributed By:</b><br> Kent Fanning<br> Dept. of Marine Science<br> University of South Florida<br> 140 Seventh Avenue, South<br> St. Petersburg, FL 33701<br> <br> phone: 727 553 1594<br> e-mail: <a href= "mailto: kaf@seas.marine.usf.edu"> kaf@seas.marine.usf.edu </a><br> <br> <i> Last updated January 13, 2006; gfh</i></pre> Nitrate, nitrite, phosphate, ammonia, and silica were measured from every niskin bottle tripped from all hydrocasts on this cruise. All concentrations are reported in micromoles per liter. <p>Analytical methods used for silica, phosphate, nitrite, and nitrate follow the recommendations of Gordon et al. (1993) for the WOCE WHP project. </p> <p>The analytical system we employ is a five-channel Technicon Autoanalyzer II upgraded with new heating baths, proportional pumps, colorimeters, improved optics, and an analog to digital conversion system (New Analyzer Program v. 2.40 by Labtronics, Inc.) This Technicon is designed for shipboard as well as laboratory use. </p> <p>Silica is determined by forming the heteropoly acid of dissolved orthosilicic acid and ammonium molybdate, reducing it with stannous chloride, and then measuring its optical transmittance.</p> <p>Phosphate is determined by creating the phosphomolybdate heteropoly acid in much the same way as with the silica method. However, its reducing agent is dihydrazine sulfate, after which its transmittance is also measured. A heating bath is required to maximize the color yield. </p> <p>Nitrite is determined essentially by the Bendschneider and Robinson (1952) technique in which nitrite is reacted with sulfanilamide (SAN) to form a diazotized derivative that is then reacted with a substituted ethylenediamine compound (NED) to form a rose pink azo dye which is measured colorimetrically. </p> <p>Nitrate is determined by difference after a separate aliquot of a sample is passed through a Cd reduction column to convert its nitrate to nitrite, followed by the measurement of the "augmented" nitrite concentration using the same method as in the nitrite analysis. </p> <p>In the analytical ammonia method, ammonium reacts with alkaline phenol and hypochlorite to form indophenolblue. Sodium nitroferricyanide intensifies the blue color formed, which is then measured in a colorimeter of our nutrient-analyzer. Precipitation of calcium and magnesium hydroxides is eliminated by the addition of sodium citrate complexing reagent. A heating bath is required. Our version of this technique is based on modifications of published methods such as the article by F. Koroleff in Grasshoff (1976). These modifications were made at Alpkem (now Astoria-Pacific International, Inc.) and at L.Gordon&#039;s nutrient laboratory at Oregon State University.</p> 10090 POC_PON POC_PON http://globec.whoi.edu/jg/serv/globec/soglobec/fullchn.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/POC_PON%7D <h2 align=center> Particulate Organic Carbon and Nitrogen<br>from Ice and Water Samples</h2> <p><b>Data Note:</b><br> This data set consists of samples derived from a varity substrats, depths within substrats and sampling devices: ice, slush, brine, water, ice core, bottles, buckets etc. The user may want to out edit the file(s) before use. <p><b>Methods:</b><br> Weight percent carbon, hydrogen, and nitrogen were determined by combustion analysis at the UCSB Marine Science Institute Analytical Laboratory (www.msi.ucsb.edu/Analab/index.html), using automated organic elemental analyzers (CHNs) manufactured by Exeter Analytical (www.eai1.com) (formerly Control Equipment Corp.), Model 440XA. Instruments were operated following manufacturer-recommended settings and procedures, and calibrated using acetanilide, with performance being monitored to achieve an analytical precision of 0.3 wt. %. (per Wendy Kozlowski, e-mail 11/23/03)<br> <p> POC and PON values have been corrected for a filtered sea water blank value of: 10.32 <i>u</i>g for POC and 1.59 <i>u</i>g for PON. </p> <p><b> A short note on the "grid":</b> The grid is a Cartesian plane covering the sample region in which distances are easy to calculate. The grid system used for SOGLOBEC is a universal transverse mercator (UTM) projection with a certain base point and rotation. The base point was chosen in the far south and the rotation was chosen to create one axis along the peninsula, and the other offshore. The units of UTM are meters, but the points are chosen in km rounded to the nearest km. Negative numbers mean that samples were taken southwest of the y axis or southeast of the x axis. For more details see: <a href="http://globec.whoi.edu/so-dir/soglobec.grid.txt"> Complete explanation of the Southern Ocean grid system. </a><p></p> <b>Data contributed by:</b><br> Maria Vernet<br> Integrative Oceanographic Division<br> Scripps Institution of Oceanography<br> University of California San Diego<br> La Jolla, California 92093-0218<br><p> Phone: 1-858-534-5322<br> E-mail: <a href="mailto:mvernet@ucsd.edu">mvernet@ucsd.edu</a><br><br><br> <i>Last updated: December 13, 2005; gfh</i></p> This data set consists of samples derived from a varity substrats, depths within substrats and sampling devices: ice, slush, brine, water, ice core, bottles, buckets etc. Weight percent carbon, hydrogen, and nitrogen were determined by combustion analysis at the UCSB Marine Science Institute Analytical Laboratory (www.msi.ucsb.edu/Analab/index.html), using automated organic elemental analyzers (CHNs) manufactured by Exeter Analytical (www.eai1.com) (formerly Control Equipment Corp.), Model 440XA. Instruments were operated following manufacturer-recommended settings and procedures, and calibrated using acetanilide, with performance being monitored to achieve an analytical precision of 0.3 wt. %. (per Wendy Kozlowski, e-mail 11/23/03)<br> </p><p> POC and PON values have been corrected for a filtered sea water blank value of: 10.32 <i>u</i>g for POC and 1.59 <i>u</i>g for PON. </p> 10091 prodPI prodPI http://globec.whoi.edu/jg/serv/globec/soglobec/fullprodpi.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/prodPI%7D <h2 align=center> Production vs Irradiance </h2><p> <p><b> A short note on the "Southern Ocean Grid System":</b> The grid is a Cartesian plane covering the sample region in which distances are easy to calculate. The grid system used for SOGLOBEC is a universal transverse mercator (UTM) projection with a certain base point and rotation. The base point was chosen in the far south and the rotation was chosen to create one axis along the peninsula, and the other offshore. The units of UTM are meters, but the points are chosen in km rounded to the nearest km. Negative numbers mean that samples were taken southwest of the y axis or southeast of the x axis. For more details see: <a href="http://globec.whoi.edu/so-dir/soglobec.grid.txt"> Complete explanation of the Southern Ocean grid system. </a><p> <p align=left> <b>Reference:</b><br> Platt, T, and Jassby, A.D., 1976. The relationship between Photosynthesis and Light for Natural Assemblages of Coastal Marine Phytoplankton. <i>Journal of Phycology</i>. <b>Vol. 12</b>; p. 421-430. </p> <p> <b>Data Contributed by:</b><br> Maria Vernet<br> Integrative Oceanographic Division<br> Scripps Institution of Oceanography<br> University of California San Diego<br> La Jolla, California 92093-0218<br><br> Phone: 1-858-534-5322<br> E-mail: <a href="mailto:mvernet@ucsd.edu">mvernet@ucsd.edu</a><br><br><br> <i>Last updated: December 01, 2005; gfh</i></p> roduction vs Irradiance data from Southern Ocean Globec for NBP0103 cruise 10092 prodSIS prodSIS http://globec.whoi.edu/jg/serv/globec/soglobec/fullprodsis.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/prodSIS%7D <h2 align=center> Simulated in Situ Primary Production Data </h2> <p><b>Data Notes:</b><br> 1..Cruise NBP0104. A total of only 6 SIS experiments were completed, due to freezing of the deck incubator. Ref: cruise report.<br> 2..PAR measurements. PAR was measured with a Biospherical Instruments GUV Radiometer (cosine-corrected downwelled irradiance) mounted on ship's science mast configured with PAR channels (400-700nm). PAR values are intergated over the duration of the in situ experiment. Ref: cruise reports<br> <p> <p><b> A short note on the "Southern Ocean Grid System":</b><br> The grid is a cartesian plane covering the sample region in which distances are easy to calculate. The grid system used for SOGLOBEC is a universal transverse mercator (UTM) projection with a certain base point and rotation. The base point was chosen in the far south and the rotation was chosen to create one axis along the peninsula, and the other offshore. The units of UTM are meters, but the points are chosen in km rounded to the nearest km. Negative numbers mean that samples were taken southwest of the y axis or southeast of the x axis. For more deatails see: <a href="http://globec.whoi.edu/so-dir/soglobec.grid.txt"> Complete explanation of the Southern Ocean grid system. </a><p> <p> <b>Reference:</b><br> Smith, R.C., H. Dierssen, and M. Vernet. in press. Phytoplankton biomass and productivity to the west of the Antarctic Peninsula. In E.Hofmann, L. Quetin, and R. Ross (Eds.), <i> Foundations for ecosystem research in the western Antarctic Peninsula region.</i> Washington, D.C.: American Geophysical Union.<br> <p> <b>Data contributed by:</b><br> Maria Vernet<br> Integrative Oceanographic Division<br> Scripps Institution of Oceanography<br> University of California San Diego<br> La Jolla, California 92093-0218<br><p> Phone: 1-858-534-5322<br> E-mail: <a href="mailto:mvernet@ucsd.edu">mvernet@ucsd.edu</a><br><br><br> <i>Last updated: December 02, 2005; gfh</i></p> <ol> <li>Cruise NBP0104. A total of only 6 SIS experiments were completed, due to freezing of the deck incubator. Ref: cruise report. <li>PAR measurements. PAR was measured with a Biospherical Instruments GUV Radiometer (cosine-corrected downwelled irradiance) mounted on ship science mast configured with PAR channels (400-700nm). PAR values are intergated over the duration of the in situ experiment. Ref: cruise reports. </ol> 10093 seaice seaice http://globec.whoi.edu/jg/serv/globec/soglobec/seaice.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seaice%7D <h3> Sea Ice Observations during Southern Ocean GLOBEC </h3> <p>Sea ice observations on the Southern Ocean GLOBEC cruises were conducted according to standardized protocols developed and utilized by members of the Antarctic Sea Ice Processes and Climate working group (co-sponsored by SCAR and GlOCHANT).</p> <p>Related datasets:<br /> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/ice_properties.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ice_properties%7D" target="_blank">ice properties</a>, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/ice_thickness.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/ice_thickness%7D" target="_blank">ice thickness</a>, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/snow_pits.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/snow_pits%7D" target="_blank">snow pits</a></p> <p>More details regarding methodology can be found at <a href="http://www.scar.org/GLOCHANT/ASPeCt/seaiceobs.htm">http://www.scar.org/GLOCHANT/ASPeCt/seaiceobs.htm</a> or by contacting Dr. C.H. Fritsen at <a href="mailto:cfritsen@dri.edu">cfritsen@dri.edu</a>.</p> <p><table width=100%> <tr><td> <p> <table align=center border> <caption><b>OPEN WATER (OpnWtrCode)</b></caption> <tr><th> Code</th><th> Description </th></tr> <tr><td>0 </td><td>No openings</td></tr> <tr><td>1 </td><td>Small cracks </td></tr> <tr><td>2 </td><td>Very narrow breaks, <50m </td></tr> <tr><td>3 </td><td>Narrow breaks, 50-200 m</td></tr> <tr><td>4 </td><td>Wide breaks, 200-500 m </td></tr> <tr><td>5 </td><td>Very wide breaks, >500 m </td></tr> <tr><td>6 </td><td>Lead/coastal lead</td></tr> <tr><td>7 </td><td>Polynya/coastal polynya </td></tr> <tr><td>8 </td><td>Water broken only by small scattered floes </td></tr> <tr><td>9 </td><td>Open sea</td></tr> </table> </td> <td> <table align=center border> <caption><b>ICE CONCn (IceCon) </b></caption> <tr><td>to be expressed in tenths </td></tr> </table> </td> </tr> </table> </p> <p> <table width=100%> <tr><td> <table align=center border> <caption><b>ICE TYPE (ITypeCode)</b></caption> <tr><th> Code</th><th> Description</th></tr> <tr><td>10</td><td> Frazil</td></tr> <tr><td>11</td><td> Shuga </td></tr> <tr><td>12 </td><td> Grease </td></tr> <tr><td> 20 </td><td> Nilas </td></tr> <tr><td> 30 </td><td> Pancakes </td></tr> <tr><td> 40 </td><td> Young grey ice, 0.1-0.15 m </td></tr> <tr><td> 50 </td><td> Young grey-white ice, 0.15-0.3 m </td></tr> <tr><td> 60 </td><td> First year, 0.3-0.7 m </td></tr> <tr><td> 70 </td><td> First year, 0.7-1.2 m </td></tr> <tr><td> 80 </td><td> First year, >1.2 m </td></tr> <tr><td> 85 </td><td> Multiyear floes </td></tr> <tr><td> 90 </td><td> Brash </td></tr> <tr><td> 95 </td><td> Fast ice </td></tr> </table> </td><td> <table align=center border> <caption><b>SEA ICE (IThkns) AND SNOWTHICKNESS (SnoThkns) </b></caption> <tr><td>to be expressed in centimetres </td></tr> </table> </td></tr> </table> </p> <p> <table width=100%> <tr><td> <table align=center border> <caption><b>FLOE SIZE (FloSzCode) </b></caption> <tr><th> Code</th><th> Description </th></tr> <tr><td>100 </td><td>Pancakes </td></tr> <tr><td>200 </td><td>New sheet ice </td></tr> <tr><td>300 </td><td>Brash/broken ice </td></tr> <tr><td>400 </td><td>Cake ice, <20 m </td></tr> <tr><td>500 </td><td>Small floes, 20-100 m </td></tr> <tr><td>600 </td><td>Medium floes, 100-500 m </td></tr> <tr><td>700 </td><td>Large floes, 500-2000 m </td></tr> <tr><td>800 </td><td>Vast floes, >2000 m </td></tr> </table> <br> <table align=center border> <caption><b>SNOW TYPE (SnoTypCode) </b></caption> <tr><th> Code</th><th> Description </th></tr> <tr><td>0 </td><td>No snow observation</td></tr> <tr><td>1 </td><td>No snow, no ice or brash </td></tr> <tr><td>2 </td><td>Cold new snow, < 1 day old </td></tr> <tr><td>3 </td><td>Cold old snow</td></tr> <tr><td>4 </td><td>Cold wind-packed snow </td></tr> <tr><td>5 </td><td>New melting snow (wet new snow) </td></tr> <tr><td>6 </td><td>Old melting snow</td></tr> <tr><td>7 </td><td>Glaze </td></tr> <tr><td>8 </td><td>Melt slush</td></tr> <tr><td>9 </td><td>Melt puddles </td></tr> <tr><td>10 </td><td>Saturated snow (waves)</td></tr> <tr><td>11 </td><td>Sastrugi</td></tr> </table> </td><td> <table align=center border> <caption><b>TOPOGRAPHY (TopoCode) </b></caption> <tr><th> Code</th><th> Description </th></tr> <tr><td>100 </td><td>Level ice</td></tr> <tr><td>200 </td><td>Rafted pancakes </td></tr> <tr><td>300</td><td> Cemented pancakes</td></tr> <tr><td>400 </td><td>Finger rafting</td></tr> <tr><td>5xy </td><td>New, unconsolidated ridges (no snow) </td></tr> <tr><td>6xy </td><td>New ridges filled with snow or a snow cover </td></tr> <tr><td>7xy </td><td>Consolidated ridges (no weathering) </td></tr> <tr><td>8xy </td><td>Older, weathered ridges </td></tr> <tr><th>x values </th><th> Areal Coverage </th></tr> <tr><td>0 </td><td>0-10% </td></tr> <tr><td>1 </td><td>10-20% </td></tr> <tr><td>2 </td><td>20-30% </td></tr> <tr><td>3 </td><td>30-40% </td></tr> <tr><td>4 </td><td>40-50% </td></tr> <tr><td>5 </td><td>50-60% </td></tr> <tr><td>6 </td><td>60-70% </td></tr> <tr><td>7 </td><td>70-80% </td></tr> <tr><td>8 </td><td>80-90% </td></tr> <tr><td>9 </td><td>90-100% </td></tr> <tr><th>y values </th><th>Avg. Sail Height</th></tr> <tr><td>1 </td><td>0.5 m </td></tr> <tr><td>2 </td><td>1.0 m </td></tr> <tr><td>3 </td><td>1.5 m </td></tr> <tr><td>4</td><td> 2.0 m </td></tr> <tr><td>5 </td><td>3.0 m </td></tr> <tr><td>6 </td><td>4.0 m </td></tr> <tr><td>7 </td><td>5.0 m</td></tr> </table> </td></tr> </table></p> <p> ¬  </p> <p><b> The following weather observation codes and descriptions are from the "National Weather Service Observing Handbook No. 1", Marine Surface Weather Observations, August 1995. U.S. Department of Commerce, Silver Spring, MD.</b></p> <p> ¬  </p> <table width=100%> <tr><td> <table align=center border> <caption><b>VISIBILITY (visib) </b></caption> <tr><th> Code</th><th> Visibility in m/km </th></tr> <tr><td>90 </td><td>less than 50 m</td></tr> <tr><td>91 </td><td>50 but less than 200 m</td></tr> <tr><td>92 </td><td>200 but less than 500 m</td></tr> <tr><td>93 </td><td>500 but less than 1000 m</td></tr> <tr><td>94 </td><td>1 but less than 2 km</td></tr> <tr><td>95 </td><td>2 but less than 4 km</td></tr> <tr><td>96 </td><td>4 but less than 10 km</td></tr> <tr><td>97 </td><td>10 but less than 20 km</td></tr> <tr><td>98 </td><td>20 but less than 50 km</td></tr> <tr><td>99 </td><td>50 km or more</td></tr> </table> <br> <p> ¬  </p> <table align=center border> <caption><b>TOTAL CLOUD COVER (cldcvr) </b></caption> <tr align=center><td> ¬  </td><td>to be expressed in eighths </td></tr> <tr><td>-1 </td><td> Sky obscured by fog, snow or other met. phenom.</td></tr> </table> <br> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> <p> ¬  </p> </td><td> <table align=center border> <caption><b>PRESENT WEATHER (wx) </b></caption> <tr><th> Code</th><th> Description</th></tr> <tr align = center><td>¬  </td><td><b> Change of sky during past hour</td></tr> <tr><td>0 </td><td>Cloud development not observable</td></tr> <tr><td>1 </td><td>Clouds dissolving or becoming less developed</td></tr> <tr><td>2 </td><td>State of the sky on the whole unchanged</td></tr> <tr><td>3 </td><td>Clouds generally forming or developing</td></tr> <tr align=center><td>¬  </td><td><b>Phenomena in past hour but not at time of obs</b></td></tr> <tr><td>28 </td><td>Fog (in past hour, but not at time of obs.)</td></tr> <tr><td>¬ </td><td>¬ </td></tr> <tr><td>36 </td><td>Slight or moderate drifting snow, low (below eye level)</td></tr> <tr><td>37 </td><td>Heavy drifting snow, low (below eye level)</td></tr> <tr><td>38 </td><td>Slight or moderate drifting snow, high (above eye level)</td></tr> <tr><td>39 </td><td>Heavy drifting snow, high (above eye level)</td></tr> <tr align=center><td>¬ </td><td><b>Fog at the time of observation</b></td></tr> <tr><td>41</td><td>Sky visible <br> Fog in patches (visibility may be greater than 1/2 nm)</td></tr> <tr><td>42</td><td>Sky visible <br> Fog has become thinner in past hour</td></tr> <tr><td>43 </td><td>Sky invisible <br>For has become thinner in past hour</td></tr> <tr><td>44 </td><td>Sky visible <br> Fog, no change in past hour</td></tr> <tr><td>45</td><td>Sky invisible <br> Fog, no change in past hour</td></tr> <tr><td>46 </td><td>Sky visible <br> Fog has begun or thickened in past hour</td></tr> <tr><td>47 </td><td>Sky invisible <br> Fog has begun or thickened in past hour</td></tr> <tr align=center><td>¬  </td><td><b>Drizzle</b></td></tr> <tr><td>50</td><td>Intermittent <br> Slight drizzle</td></tr> <tr><td>56 </td><td>Slight <br> Freezing drizzle</td></tr> <tr align=center><td>¬ </td><td><b> Rain (Not falling as showers)</b></td></tr> <tr><td>60 </td><td>Intermittent <br> Slight rain</td></tr> <tr align=center><td>¬ </td><td><b>Solid precipitation not falling as showers</b></td></tr> <tr><td>70</td><td>Intermittent <br> Slight snow in flakes</td></tr> <tr><td>71</td><td>Continuous <br> Slight snow in flakes</td></tr> <tr><td>72</td><td>Intermittent <br> Moderate snow in flakes</td></tr> <tr><td>73 </td><td>Continuous <br> Moderate snow in flakes</td></tr> <tr><td>74 </td><td>Intermittent <br> Heavy snow in flakes</td></tr> <tr><td>75</td><td>Continuous <br> Heavy snow in flakes</td></tr> <tr><td>76 </td><td>Diamond dust (with or without fog)</td></tr> <tr><td>77 </td><td>Snow grains (with or without fog)</td></tr> <tr align=center><td>¬  </td><td><b>Solid precipitation in showers</b></td></tr> <tr><td>85</td><td>Slight <br> Shower of snow</td></tr> <tr><td>86</td><td>Moderate or heavy <br> Shower of snow</td></tr> </table> </td></tr> </table> </p> </pre> <p>Sea ice observations on the Southern Ocean GLOBEC cruises were conducted according to standardized protocols developed and utilized by members of the Antarctic Sea Ice Processes and Climate working group (co-sponsored by SCAR and GlOCHANT).</p> <p>Routine observations of sea ice and snow characteristics were routinely collected on an hourly basis while the <em>L.M. Gould</em> was actively steaming throughout the cruise. These observations began on 26 July 2001 and continued through 27 August 2001. The observational protocol followed during the cruise was the protocol that is formally endorsed by the SCAR ASPeCt (Antarctic Sea ice Processes and Climate) program for observing sea ice characteristics. In short, our program (combined efforts of BG-244 as well as OG-241) was able to gather the information that will be used to characterize the predominate types of ice in the region according to parameters, such as areal coverage, floe size, ice thickness, snow type, snow thickness and deformation.</p> More details regarding methodology can be found at <a href="http://www.scar.org/GLOCHANT/ASPeCt/seaiceobs.htm">http://www.scar.org/GLOCHANT/ASPeCt/seaiceobs.htm</a> or by contacting Dr. C.H. Fritsen at <a href="mailto:cfritsen@dri.edu">cfritsen@dri.edu</a>. 10094 seals_general seals_general http://globec.whoi.edu/jg/serv/globec/soglobec/seals_general.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_general%7D <h3 align=center> Seal Studies, Southern Ocean GLOBEC,<br> General Seal Metadata</h3> <p> <b>Reference:</b> <a href="http://globec.whoi.edu/globec-dir/Laws.pdf">Laws, R. M., Baird A., Bryden M. M., 2003.</a> Size and growth of the crabeater seal <i>Lobodon carcinophagus</i> (Mammalia: Carnivora). Journal of Zoology (London) <b>259</b>, 103-108. </p> <b>For additional details on sampling and analytical methods see:</b><br> Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. <a href ="http://dx.doi.org/10.1016/j.dsr2.2004.07.021">Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula.</a> Deep-Sea Research II vol 51, pp 2279-2303.<p><br> <b>Links to companion seal files:</b><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_phys.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_phys%7D">Seal Physiology</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_morphs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_morphs%7D">Seal Morphometrics</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_predmass.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_predmass%7D">Seal Predicted Mass</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_loc_test.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_loc%7D">Seal Tracking Locations From Satellite Tags</a><br><br> <p><b>Contact Information:</b><br> Jennifer Burns, Ph.D.<br> Department of Biological Sciences<br> University of Alaska<br> Anchorage, AK 99508<br> 907-786-1527<br> <a href="mailto:afjmb4@uaa.alaska.edu">afjmb4@uaa.alaska.edu</a></p> <p> Daniel P. Costa Ph.D.<br> Long Marine Laboratory<br> University of California<br> 100 Shaffer Rd<br> Santa Cruz, CA 95060<br> Office: 831 459-2786<br> FAX: 831 459-3383<br> <a href="mailto:costa@biology.ucsc.edu">costa@biology.ucsc.edu</a></p> <p> <i> last updated April 25, 2006 </i> Seal Studies, Southern Ocean GLOBEC, General Seal Metadata. <b>For additional details on sampling and analytical methods see:</b><br>Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. <a href=&#039;http://dx.doi.org/10.1016/j.dsr2.2004.07.021&#039;>Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula.</a> Deep-Sea Research II vol 51, pp 2279-2303.<p><br> 10095 seals_phys seals_phys http://globec.whoi.edu/jg/serv/globec/soglobec/seals_phys.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_phys%7D <h3 align=center> Seal Studies, Southern Ocean GLOBEC,<br> Seal Physiology Data </h3> <p> <b>For additional details on sampling and analytical methods see:</b><br> Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula. Deep-Sea Research II vol 51, pp 2279-2303. <p><br> <b>Links to companion seal files:</b><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_general.html0%7Bdir=globec.whoi.edu/ jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_general%7D">General Seal Background Information</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_morphs.html0%7Bdir=globec.whoi.edu/j g/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_morphs%7D">Seal Morphometrics</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_predmass.html0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_predmass%7D">Seal Predicted Mass</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_loc_test.brev0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_loc%7D">Seal Tracking Locations From Satellite Tags</a><br><br> <p><b>Contact Information:</b><br> Jennifer Burns, Ph.D.<br> Department of Biological Sciences<br> University of Alaska<br> Anchorage, AK 99508<br> 907-786-1527<br> <a href="mailto:afjmb4@uaa.alaska.edu">afjmb4@uaa.alaska.edu</a></p> <p> Daniel P. Costa Ph.D.<br> Long Marine Laboratory<br> University of California<br> 100 Shaffer Rd<br> Santa Cruz, CA 95060<br> Office: 831 459-2786<br> FAX: 831 459-3383<br> <a href="mailto:costa@biology.ucsc.edu">costa@biology.ucsc.edu</a></p> <p> <i> last updated April 25, 2006</i> 10096 seals_morphs seals_morphs http://globec.whoi.edu/jg/serv/globec/soglobec/seals_morphs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_morphs%7D <h3 align=center> Seal Studies, Southern Ocean GLOBEC,<br> Seal Morphometrics Data</h3> <p><b>*</b> Blubber depths determined by ultrasound <br><br> <b>For additional details on sampling and analytical methods see:</b><br> Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula. Deep-Sea Research II vol 51, pp 2279-2303. </p><br> <b>Links to companion seal files:</b><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_general.html0%7Bdir=globec.whoi.edu/ jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_general%7D">General Seal Background Information</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_phys.html0%7Bdir=globec.whoi.edu/jg/ dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_phys%7D">Seal Physiology</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_predmass.html0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_predmass%7D">Seal Predicted Mass</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_loc_test.brev0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_loc%7D">Seal Tracking Locations From Satellite Tags</a></p><br> </p> <p><b>Contact Information:</b><br> Jennifer Burns, Ph.D.<br> Department of Biological Sciences<br> University of Alaska<br> Anchorage, AK 99508<br> 907-786-1527<br> <a href="mailto:afjmb4@uaa.alaska.edu">afjmb4@uaa.alaska.edu</a></p> <p> Daniel P. Costa Ph.D.<br> Long Marine Laboratory<br> University of California<br> 100 Shaffer Rd<br> Santa Cruz, CA 95060<br> Office: 831 459-2786<br> FAX: 831 459-3383<br> <a href="mailto:costa@biology.ucsc.edu">costa@biology.ucsc.edu</a></p><br> <i>last updated April 25, 2006</i> 10097 seals_predmass seals_predmass http://globec.whoi.edu/jg/serv/globec/soglobec/seals_predmass.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_predmass%7D <h3 align=center> Seal Studies, Southern Ocean GLOBEC,<br> Predicted Mass & Age Data </h3> <p> <b>Reference:</b> <a href="http://globec.whoi.edu/globec-dir/Laws.pdf">Laws, R. M., Baird A., Bryden M. M., 2003.</a> Size and growth of the crabeater seal <i>Lobodon carcinophagus</i> (Mammalia: Carnivora). Journal of Zoology (London) <b>259</b>, 103-108. </p> <p> <b>For additional details on sampling and analytical methods see:</b><br> Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. <a href ="http://dx.doi.org/10.1016/j.dsr2.2004.07.021">Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula.</a> Deep-Sea Research II vol 51, pp 2279-2303.<p> <b>Links to companion seal files:</b><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_general.html0%7Bdir=globec.whoi.edu/ jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_general%7D">General Seal Background Information</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_phys.html0%7Bdir=globec.whoi.edu/jg/ dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_phys%7D">Seal Physiology</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_morphs.html0%7Bdir=globec.whoi.edu/j g/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_morphs%7D">Seal Morphometrics</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_loc_test.brev0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_loc%7D">Seal Tracking Locations From Satellite Tags</a></p><br> <p><b>Contact Information:</b><br> Jennifer Burns, Ph.D.<br> Department of Biological Sciences<br> University of Alaska<br> Anchorage, AK 99508<br> 907-786-1527<br> <a href="mailto:afjmb4@uaa.alaska.edu">afjmb4@uaa.alaska.edu</a></p> <p> Daniel P. Costa Ph.D.<br> Long Marine Laboratory<br> University of California<br> 100 Shaffer Rd<br> Santa Cruz, CA 95060<br> Office: 831 459-2786<br> FAX: 831 459-3383<br> <a href="mailto:costa@biology.ucsc.edu">costa@biology.ucsc.edu</a></p><br> <i>Last updated April 25, 2006</i> Seal Studies, Southern Ocean GLOBEC, Predicted Mass & Age Data. <b>For additional details on sampling and analytical methods see:</b><br>Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. <a href=&#039;http://dx.doi.org/10.1016/j.dsr2.2004.07.021&#039;>Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula.</a> Deep-Sea Research II vol 51, pp 2279-2303.<p><br> 10098 seals_loc seals_loc http://globec.whoi.edu/jg/serv/globec/soglobec/seals_loc_test.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_loc%7D <h3 align=center> Tagged Seal Location Data from SOGLOBEC</h3> <p> <b>For additional details on sampling and analytical methods see:</b><br> Burns, Jennifer M., Daniel P. Costa, Michael A. Fedak, Mark A. Hindell, Corey J.A. Bradshaw, Nicholas C. Gales, Birgitte McDonald, Stephan J. Trumble, Daniel E. Crocker, 2004. <a href ="http://dx.doi.org/10.1016/j.dsr2.2004.07.021">Winter habitat use and foraging behavior of crabeater seals along the Western Antarctic Peninsula.</a> Deep-Sea Research II vol 51, pp 2279-2303. <br> <p> <b>Links to companion seal files:</b><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_general.html0%7Bdir=globec.whoi.edu/ jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_general%7D">General Seal Background Information</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_phys.html0%7Bdir=globec.whoi.edu/jg/ dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_phys%7D">Seal Physiology</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_morphs.html0%7Bdir=globec.whoi.edu/j g/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_morphs%7D">Seal Morphometrics</a><br> <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/seals_predmass.html0%7Bdir=globec.whoi.edu /jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/seals_predmass%7D">Seal Predicted Mass</a><br></p> <hr> </p> <p><b>Contact Information:</b><br> Jennifer Burns, Ph.D.<br> Department of Biological Sciences<br> University of Alaska<br> Anchorage, AK 99508<br> 907-786-1527<br> <a href="mailto:afjmb4@uaa.alaska.edu">afjmb4@uaa.alaska.edu</a></p> <p> Daniel P. Costa Ph.D.<br> Long Marine Laboratory<br> University of California<br> 100 Shaffer Rd<br> Santa Cruz, CA 95060<br> Office: 831 459-2786<br> FAX: 831 459-3383<br> <a href="mailto:costa@biology.ucsc.edu">costa@biology.ucsc.edu</a></p><br> <i>Last updated February 17, 2006</i> 10099 simrad simrad http://globec.whoi.edu/jg/serv/globec/soglobec/simrad.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/simrad%7D <h3 align=center>Information file for processing and plotting simrad files</h3> <p>The original telegrams from the simrad EK500 for 38, 120, 200 kHz transducers are transmitted to RVDAS via RS232 at 115kb and logged daily with a new file started at 0000 GMT (2000 h local). To process the raw simrad output, the perl script <a href="http://globec.whoi.edu/so-dir/data/simandmwaythen.pl"> simandmwaythen.pl</a> (written by Karen Fisher) picks up the day.dat file, which must be set by the user, and loads and outputs a series of files for each frequency and time. The matlab m file, <a href="http://globec.whoi.edu/so-dir/data/simthenplotter_2.m">simthenplotter_2.m</a>, picks up the output from the perl script, plots and then saves mat files. The m file called <a href="http://globec.whoi.edu/so-dir/data/plotsimrad.m">plotsimrad.m</a> asks you for the matlab filename and plots the output.</p> <p>All the matlab files for each day of NBP0204 are available in gz zipped format. All the user needs to do is to unzip the mat file of choice, and run plotsimrad.m. You do not need to go back to the raw data if you just wish to plot data for a particular day or time window. The data in the *.mat files are corrected for the offset produced by the noise margin setting on the simrad and calibrated by cross correlation with data from biomaperII when it was in the water at the same time. This is not a true calibration since the accuracy is unknown, but it probably gives correct backscatter intensity within a few db. The range is -100 to -40 and color scaled (thanks to Gareth Lawson) in the plots just as in the output from biomaperII.</p> <p>plotsimrad.m allows you to select the times within a given day to plot so you can "zoom in" on specific activites such as CTD or MOCNESS casts. The perl script is made available in case the user wishes to go back to the raw data and re-process for some reason. There is also have a script to cross plot backscatter intensity against temperature gradient data from the CTD and CMIPS during each cast. Contact Scott Gallager if you are interested.</p> <p><b>Note about downloading the above program files:</b> <br> When you click on the above links, the perl script and the matlab files may be output to your browser window. To download them, use 'save as' at your browser's file menu. You can avoid the screen output and download directly by <u>first</u> holding the 'shift' key and <u>then</u> clicking on the link.</p> <p>Other helpful files: <br> <a href="http://globec.whoi.edu/so-dir/data/simrad_data/cmap.m">cmap.m</a> <br> <a href="http://globec.whoi.edu/so-dir/data/simrad_data/initialize_simradplot.m">initialize_simradplot.m</a> </p> <i>16 sept 2002 <br> Scott Gallager<br> sgallager@whoi.edu</i> The original telegrams from the simrad EK500 for 38, 120, 200 kHz transducers are transmitted to RVDAS via RS232 at 115kb and logged daily with a new file started at 0000 GMT (2000 h local). To process the raw simrad output, the perl script <a href="http://globec.whoi.edu/so-dir/data/simandmwaythen.pl"> simandmwaythen.pl</a> (written by Karen Fisher) picks up the day.dat file, which must be set by the user, and loads and outputs a series of files for each frequency and time. The matlab m file, <a href="http://globec.whoi.edu/so-dir/data/simthenplotter_2.m">simthenplotter_2.m</a>, picks up the output from the perl script, plots and then saves mat files. The m file called <a href="http://globec.whoi.edu/so-dir/data/plotsimrad.m">plotsimrad.m</a> asks you for the matlab filename and plots the output. 10100 sonobuoy_whale sonobuoy_whale http://globec.whoi.edu/jg/serv/globec/soglobec/sonobuoy_whale.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/sonobuoy_whale%7D <b>Working Procedure:</b><br> A sonobuoy is deployed and monitored until it is out of range. The length of time the sonobuoy can be heard depends on the speed of the ship, the sonobuoy's direction relative to the ship and the prevailing sea, ice and weather conditions. When a whale is heard, an attempt is made to identify the species and note it. If a seal is heard, it is just noted as a seal. The sonobuoy was set to scuttle after 8 hours. </p><br> <p> <b> Questions regarding these data should be directed to:</b><br> John Hildebrand <br> Scripps Institution of Oceanography, UCSD <br> 9500 Gilman Drive <br> La Jolla CA, 92093-0205 <br><br> Email: jhildebrand@ucsd.edu <br><br> <i> Last Updated February 22, 2006 </i></p> A sonobuoy is deployed and monitored until it is out of range. The length of time the sonobuoy can be heard depends on the speed of the ship, the sonobuoy&#039;s direction relative to the ship and the prevailing sea, ice and weather conditions. When a whale is heard, an attempt is made to identify the species and note it. If a seal is heard, it is just noted as a seal. The sonobuoy was set to scuttle after 8 hours. 10101 sv120data sv120data http://globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120data.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/sv120data%7D <p>These relative decibel values are the result of processing the NBP0104 and NBP0103 volume backscatter data from BIOMAPER-II at 120KHz. They are relative decibel values derived from the backscatter data (in volts) and normalized according to the algorithms in the Matlab routine docurtainnf.m. The algorithm includes the following steps:<p> <ol> <li>Add 10^-10 to each value</li> <li>Multiply result by by 10¹⁰ to get values with units of m²/m³ (called sv) <li>Take the log (called SV)</li> </ol> <p> These are energy backscattering values. <p> The values are presented as twenty groups of 20 numbers in each group. Each number is displayed as NNN, where there is an assumed decimal point at NN.N and all values should be negated. That is NNN, is really -NN.N. <p> See the related objects <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120coords_0104{dir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120coords_0104.brev0}"> sv120coords_0104</a> and <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120depths_0104{dir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120depths_0104.brev0}"> sv120depths_0104</a> for NBP0104 and <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120amcoords_0103{dir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120amcoords_0103.brev0}"> sv120amcoords_0103</a>, <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120pmcoords_0103{dir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120pmcoords_0103.brev0}"> sv120pmcoords_0103</a> and <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120depths_0103{dir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120depths_0103.brev0}"> sv120depths_0103</a> for NBP0103. </pre> <p>These relative decibel values are the result of processing the NBP0104 and NBP0103 volume backscatter data from BIOMAPER-II at 120KHz. They are relative decibel values derived from the backscatter data (in volts) and normalized according to the algorithms in the Matlab routine docurtainnf.m. The algorithm includes the following steps:</p><p> </p><ol> <li>Add 10^-10 to each value</li> <li>Multiply result by by 10¹⁰ to get values with units of m²/m³ (called sv) </li><li>Take the log (called SV)</li> </ol> <p> These are energy backscattering values. </p><p> The values are presented as twenty groups of 20 numbers in each group. Each number is displayed as NNN, where there is an assumed decimal point at NN.N and all values should be negated. That is NNN, is really -NN.N. See the related objects <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120amcoords_0103%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120amcoords_0103.brev0%7D"> sv120amcoords_0103</a>, <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120pmcoords_0103%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120pmcoords_0103.brev0%7D"> sv120pmcoords_0103</a> and <a href="http://globec.whoi.edu/jg/info/globec/soglobec/broadscale/2001/sv120depths_0103%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/broadscale/2001/,data=globec.whoi.edu/jg/serv/globec/soglobec/broadscale/2001/sv120depths_0103.brev0%7D"> sv120depths_0103</a> for NBP0103. 10102 zooabund_lmg zooabund_lmg http://globec.whoi.edu/jg/serv/globec/soglobec/zooabund_lmg.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/zooabund_lmg%7D <h3 align=center> Zooplankton Abundance Based on Taxa and Life Stages or Size </h3> <h3 align=center>Collected during the Process Cruises, Austral Autumn 2001 and 2002</h3> <p><b>Data Contributed By:</b><br /> Kendra L. Daly <br /> College of Marine Science<br /> University of South Florida<br /> 140 Seventh Ave. S.<br /> St. Petersburg, FL 33701<br /> <br /> Phone: 727-553-1041<br /> E-Mail: <a href= "mailto: kdaly@marine.usf.edu">kdaly@marine.usf.edu</a> </p> <p>Net sample collections: Meng Zhou, Yiwu Zhu, Ryan Dorland, Dan Mertes, and Joe Smith </p> <p>Sample Analyses: Jason Zimmerman, Alexander Timonin, Tatjana Semenova</p> <p>Zooplankton abundance, vertical and horizontal distribution, and population structure were assessed using a 1 m² Multiple Opening and Closing Nets and Environmental Sampling System (MOCNESS) with nine nets having 333<i>u</i>m mesh and environmental sensors of temperature, salinity and depth. The entire water column was sampled on the downcast using net # 0, which was not analyzed. The upper water column was typically sampled using nets 1 and 2 from 500 m to 200 m at 150 m depth intervals, nets 3 and 4 from 200 m to 100 m at 50 m depth intervals, and nets 5 to 8 from 100 m to the surface at 25 m depth intervals. Some tows were deployed down to 1000 m, and some tows were towed targeting krill swarms at irregular depths. Approximate locations of process study stations are shown in <a href="#Figure1">Fig. 1</a>. More precise locations of the casts in <a href="#fig2">Fig. 2</a>.</p> <p align="center"><a name="Figure1" id="Figure1"></a><img width=581 height=464 src="http://globec.whoi.edu/images/image002kdaly.gif"> </p> <p>Fig. 1. Approximate locations of process cruise stations in Marguerite Bay during austral autumn 2001 and 2002.</p> <p align="center"><a name="fig2" id="fig2"></a><a href="http://globec.whoi.edu/images/MOC_station_map_LMG.png"><img src="http://globec.whoi.edu/images/MOC_station_map_LMG.png" alt="MOCNESS station map" width="629" height="406" /></a></p> <p>Fig. 2. Locations of MOCNESS stations for LMGould-0104 (2001) and LMGould-0203 (2002) cruises. Numbers correspond to the cast number.</p> <p>Zooplankton samples were immediately preserved in 10% buffered formalin solution. All the large organisms (>15 mm) in the sample were removed and identified to taxa. The sample was then split to about 100 individuals of euphausiids. All euphausiids in the split were identified to species and life history stage and measured for length to the nearest 0.5 mm for larvae and to the nearest 1.0 mm for juvenile and adults. Next the sample was split to about 100 individuals of copepods. Copepods were identified to species and life history stage (female, male, copepodite V, or other copepodite). All other zooplankton in the split were identified to taxa and counted. For the Euchaetidae, we followed the designation of Park (1994) who ascribed the Antarctic species to the genus <i>Paraeuchaeta</i>. This data object ("krill") reports the abundance of each euphausiid species by life stage and size class. The companion data object "zooabund" reports the counts of zooplankton per subsample/split by taxa and life stage or size class. </p> <p>Greenwich Mean Time was local time + 4 hours.</p> <p>Reference:</p> <blockquote> <p>Park, T. 1994. Taxonomy and distribution of the marine calanoid copepod family Euchaetidae. Bulletin of the Scripps Institution of Oceanography University of California, San Diego v. 29, University of California Press, Berkeley, CA, 203 pp. </p> </blockquote> <p><strong>Notes on Volume Filtered values:</strong></p> <p>The 1 m2 MOCNESS net volume filtered data were corrected for the following net tows:</p> <p>The flowmeter used to calculate the volume of water filtered <b>did not work</b> for the tows shown below; the data shown in the listings for those tows are therefore <b>derived, not measured</b>. Using the net distance and the average angle of the net, the volume filtered was estimated. These estimates have about a 10% error or higher when currents were present. </p> <p>2001. No further corrections. MOC-1 net volume filtered values were used to calculate abundance/m3 for all net tows. No Optical Plankton Counter (OPC) volume filtered values were available for 2001.</p> <p>2002. The flowmeter data was not accurate for some net tows in 2002. Optical Plankton Counter (OPC) volume filtered was used to calculate abundance/m3 for all MOC-1 net tows, except casts 11 and 16 which used the MOC-1 volume filtered values. The decision to use OPC values was determined by plotting all OPC volume filtered numbers versus MOC-1 flow meter data (see below). MOC-1 flow meter data were consistently lower and had a lower R2 regression for volume filtered versus length of tow (time). Meng Zhou and Yiwi Zhu, who conducted the MOC-1 net tows, noted on the haul sheets that there were problems with the MOC-1 flow meters and that they often were not responsive or worked intermittently. Thus, it was decided that the OPC flow meter data provided a more consistent measure of net flow volume for 2002 net tows. The OPC mouth opening for flow meter data was corrected to the MOC-1 net mouth opening by multiplying the OPC flow data by 200. The two casts that used MOC-1 flow meter data were cases where the OPC flow meter data appeared to underestimate the flow.</p> <p align="center"><img src="http://globec.whoi.edu/images/kdaly_volfilt_info4.png" alt="LMG0202 volume filtered: MOC and OPC" width="586" height="384" /> </p> <p align="center">Fig. 3. Volume filtered over time for both MOCNESS and Optical Plankton Counter showing consistently lower flow rates for the MOCNESS.</p> <p><strong>Notes on missing samples: </strong> <p>LMG0104 - Station 1A, tow 1, net 2: non-quatitative sample<br> LMG0104 - Station 1A, tow 1, net 8: no sample <p><strong><a href="kdaly_dmo-notes.html">DMO Note</a></strong> <p><span class="style1"><i>Updated October 8, 2004; G. Heimerdinger<br /> Updated July 31, 2008; N. Copley</i></span></p> <pre> 10103 zooabund_nbp zooabund_nbp http://globec.whoi.edu/jg/serv/globec/soglobec/zooabund_nbp.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/zooabund_nbp%7D? <h3 align=center> Zooplankton Abundance Based on Taxa and Life Stages or Size Classes,<br> Collected during the Broadscale <i>NB Palmer</i> Cruises,<br> Austral Autumn 2001 and 2002<br> </h3> <p> The MOCNESS-1 plankton sampler has nine rectangular nets (1m x 1.4 m) with a mesh size of 0.333 mm, which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe et al., 1976).</br> Note: NBP0104 tows 1-11 used a 500 micron mesh for net 1 samples. Then it was moved to net 0 for remainder of tows. </p> <p><b>Cruises:</b><br> Nathaniel B. Palmer, April-June 2001 (NBP01-03), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0103,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, July-Sept. 2001 (NBP01-04), 17 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0104,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, April-May 2002 (NBP02-02), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0202,data_type%20eq%20cruise_report"> cruise report</a> <br> Nathaniel B. Palmer, July-Sept. 2002 (NBP02-04), 19 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0204,data_type%20eq%20cruise_report"> cruise report</a></p> <p>¹<b>Displacement volume measurement:</b><br> Entire sample plus liquid was measured in a large graduated cylinder then poured through a sieve into a second cylinder. The difference in volume is the displacement volume. </p> <p><b>Methods:</b></p> <p>Zooplankton abundance, vertical and horizontal distribution, and population structure were assessed using a 1 m² Multiple Opening and Closing Nets and Environmental Sampling System (MOCNESS) with nine nets having 333 µm mesh and environmental sensors of temperature, salinity and depth. The entire water column was sampled on the downcast using net # 0, which was not analyzed here. The water column was typically sampled from close to the bottom at stations on the shelf where depths were less than 1000 m, or to 1000m at stations off the shelf where depths were often from 3000 to 4000 m. Nets 1 through 8 sampled from various depth intervals to the surface with smaller strata near the surface. Several tows targeted krill swarms by towing in a single strata. Approximate locations of broadscale study stations are shown in <a href="#Figure1">Figs. 1-4</a>. </p> <p>Zooplankton samples were immediately preserved in 5% buffered formalin solution. In 2006, the samples were sent to the Atlantic Reference Centre, <a href="http://www.huntsmanmarine.ca/research_menu.shtml" target="_blank">Huntsman Marine Science Centre</a>, St. Andrews, New Brunswick, Canada to be sorted. All the large organisms (>15 mm) in the sample were removed and identified to taxa. The sample was then split to about 100 individuals of euphausiids. All euphausiids in the split were identified to species and life history stage. Next, the sample was split to about 100 individuals of copepods. Copepods were identified to species and life history stage (female, male, copepodite V, or other copepodite). All other zooplankton in the split were identified to taxa and counted. For the <i>Euchaetidae</i>, we followed the designation of Park (1994) who ascribed the Antarctic species to the genus <i>Paraeuchaeta</i>. This data object ("zooabund_nbp") reports the counts of zooplankton per subsample/split by taxa and life stage or size class. The companion data object "zooabund_lmg" reports similar for the MOCNESS samples collected on the L.M. Gould cruises and data object "krill" reports the abundance of each euphausiid species by life stage and size class, also on the L. M. Gould.</p> <p>Greenwich Mean Time was local time + 4 hours.</p> <p><b>See companion data files:</b><br> 1. <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/mocness_biovols_rs.html0{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/mocness_biovols}"> Zooplankton biovolume values from MOCNESS tows </a> - this data set is derived from displacement volume measurements and dry weight conversion calculations from the same set of samples as the above data.</p> <p> 2. <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/zoo_moc.html0{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/zoo_moc}?"> Zooplankton Abundance and biomass from MOCNESS nets using silhouette analysis</a><br> NB Palmer, austral fall &amp; winter of 2001 &amp; 2002 - Biomass (wet weight) and abundance were determined principally by silhouette digitization of taxa lengths and conversion to equivalent wet weights according to the equations and methods adapted from Davis and Wiebe (1985) and Wiebe et al. (2004).</p> <p><b>Contact Information:</b><br> Net sample collections: <a href="mailto:cashjian@whoi.edu"> Carin Ashjian</a>, <a href="mailto:pwiebe@whoi.edu"> Peter Wiebe</a>, <a href="mailto:ncopley@whoi.edu"> Nancy Copley</a>, <a href="mailto:palatalo@whoi.edu"> Phil Alatalo</a> at Woods Hole Oceanographic Inst.</p> <p>Sample Analyses: <a href="http://www.huntsmanmarine.ca/arc.shtml" target="_blank"> Atlantic Reference Centre</a> (ARC), located in St. Andrews, New Brunswick, Canada under the supervision of <a href="mailto:ARC@mar.dfo-mpo.gc.ca">Dr. Gerhard Pohle</a>.</p> <p><b>Reference:<br> </b>Davis, C.S., Wiebe, P.H., 1985. Macrozooplankton biomass in a warm-core Gulf Stream ring: Time series changes in size structure, taxonomic composition, and vertical distribution. Journal of Geophysical Research 90, 8871-8882.</p> <p>Park, T. 1994. Geographic distribution of the bathypelagic genus <i>Paraeuchaeta</i> (Copepoda, Calanoida), Hydrobiologia 292/293, 317-332.&nbsp;</p> <p><a name=Figure1>Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. Journal of Marine Research, 34(3): 313-326.<br> <br> Wiebe, P.H., C. J. Ashjian, S. M. Gallager, C. S. Davis, G. L. Lawson, and N. J. Copley. 2004. Using a high powered strobe light to increase the catch of Antarctic krill. Marine Biology. 144(3): 493 - 502.</a> </p> <p><a href="http://globec.whoi.edu/images/NBP0103_TowPositions.png"><img border="0" src="http://globec.whoi.edu/images/NBP0103_TowPositions.png" alt="NBP0103_TowPositions.png (48567 bytes)" width="400" height="425"></a> <p>Fig. 1. NBP-0103: Locations for the oblique MOCNESS tows taken in austral fall 2001 as part of the broad-scale survey (solid dots) and the horizontal tows taken in krill patches in Marguerite Bay (asterisks).</p> <p><a href="http://globec.whoi.edu/images/NBP0104_TowPositions.png"><img border="0" src="http://globec.whoi.edu/images/NBP0104_TowPositions.png" alt="NBP0104_TowPositions.png (45120 bytes)" width="400" height="425"></a></p> <p>Fig. 2. NBP-0104: Locations for the oblique MOCNESS tows taken in austral winter 2001 as part of the broad-scale survey.</p> <p><a href="http://globec.whoi.edu/images/NBP0202_TowPositions.png"><img border="0" src="http://globec.whoi.edu/images/NBP0202_TowPositions.png" alt="NBP0202_TowPositions.png (46096 bytes)" width="400" height="425"></a></p> <p>Fig. 3. NBP-0202: Locations for the oblique MOCNESS tows taken in austral fall 2002 as part of the broad-scale survey.</p> <p><a href="http://globec.whoi.edu/images/NBP0204_TowPositions.png"><img border="0" src="http://globec.whoi.edu/images/NBP0204_TowPositions.png" alt="NBP0204_TowPositions.png (45602 bytes)" width="400" height="425"></a></p> <p>Fig. 4. NBP-0204: Locations for the oblique MOCNESS tows taken in austral winter 2002 as part of the broad-scale survey.</p> <p><i>last updated: 12 Sept. 2006; gfh</i></p> Zooplankton abundance, vertical and horizontal distribution, and population structure were assessed using a 1 m2 Multiple Opening and Closing Nets and Environmental Sampling System (MOCNESS) with nine nets having 333 µm mesh and environmental sensors of temperature, salinity and depth. The entire water column was sampled on the downcast using net # 0, which was not analyzed here. The water column was typically sampled from close to the bottom at stations on the shelf where depths were less than 1000 m, or to 1000m at stations off the shelf where depths were often from 3000 to 4000 m. Nets 1 through 8 sampled from various depth intervals to the surface with smaller strata near the surface. Several tows targeted krill swarms by towing in a single strata. Zooplankton samples were immediately preserved in 5% buffered formalin solution. In 2006, the samples were sent to the Atlantic Reference Centre, Huntsman Marine Science Centre, St. Andrews, New Brunswick, Canada to be sorted. All the large organisms (>15 mm) in the sample were removed and identified to taxa. The sample was then split to about 100 individuals of euphausiids. All euphausiids in the split were identified to species and life history stage. Next, the sample was split to about 100 individuals of copepods. Copepods were identified to species and life history stage (female, male, copepodite V, or other copepodite). All other zooplankton in the split were identified to taxa and counted. For the Euchaetidae, we followed the designation of Park (1994) who ascribed the Antarctic species to the genus Paraeuchaeta. This data object (&#039;zooabund_nbp&#039;) reports the counts of zooplankton per subsample/split by taxa and life stage or size class. The companion data object &#039;zooabund_lmg&#039; reports similar for the MOCNESS samples collected on the L.M. Gould cruises and data object &#039;krill&#039; reports the abundance of each euphausiid species by life stage and size class, also on the L. M. Gould. 10104 ctd_mocness10 ctd_mocness10 http://globec.whoi.edu/jg/serv/globec/soglobec/mocness_ctd.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/mocness_ctd%7D? <h2 align=center> CTD observations taken simultaneously during MOCNESS tows, <br> plus MOCNESS sampling conditions </h2> <p> <b>Note:</b> Some variables have been eliminated from the display but are nevertheless available. These variables include: oxycurrent, oxytemp, tempco, and echo.</p> <p> The MOCNESS is based on the Tucker Trawl principle (Tucker, 1951). The particular MOCNESS system from which these CTD data came is one of two net systems. The MOCNESS-1 has nine rectangular nets (1m x 1.4 m) which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976). The MOCNESS-10 (with 10 m² nets)carries 6 nets of 3.0-mm circular mesh. In both systems, "the underwater unit sends a data frame, comprised of temperature, depth, conductivity, net-frame angle, flow count, time, number of open net, and net opening/closing, to the deck unit in a compressed hexadecimal format every 2 seconds and from the deck unit to a microcomputer every 4 seconds... Temperature (to approximately 0.01 deg C) and conductivity are measured with SEABIRD sensors. Normally, a modified T.S.K.-flowmeter is used... Both the temperature and conductivity sensors and the flow meter are mounted on top of the frame so that they face horizontally when the frame is at a towing angle of 45deg... Calculations of salinity (to approximately 0.01 o/oo S), potential temperature (theta), potential density (sigma), the oblique and vertical velocities of the net, and the approximate volume filtered by each net are made after each string of data has been received by the computer." (Wiebe <i>et al.</i>, 1985) In addition, data were collected from four other sensors attached to the frame: the Transmissometer, the Fluorometer, the Down welling light sensor, and the Oxygen sensor. A SeaBird underwater pump was also included in the sensor suite. </p> <p> It should be noted that due to Antarctic cold, the first few minutes of data are often of questionable value as they are extremely variable and have a high frequency of '50.000' (indicating 'bad values') in the temp, theta and sal fields. Once the sensors encounter deeper, warmer water, they start recording good values. </p> <p>For additional information, contact the <a href="http://usjgofs.whoi.edu/jg/serv/globec/soglobec/inventory.html0?project,name_prin"> chief scientist</a> for the cruise. <p> <h2>References</h2> <p> ¬¹Fofonoff and Millard, 1983, UNESCO technical papers in Marine Sciences, #44 </p> <p> Tucker, G.H., 1951. Relation of fishes and other organisms to the scattering of underwater sound. <i> Journal of Marine Research</i>, <b>10:</b> 215-238. </p> <p> Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. <i>Journal of Marine Research</i>, <b>34(3):</b> 313-326 </p> <p> Wiebe, P.H., A.W. Morton, A.M. Bradley, R.H. Backus, J.E. Craddock, V. Barber, T.J. Cowles and G.R. Flierl, 1985. New developments in the MOCNESS, an apparatus for sampling zooplankton and micronekton. <i>Marine Biology</i>, <b>87:</b> 313-323. </p> <i> last updated January 10, 2006; gfh</i> The MOCNESS is based on the Tucker Trawl principle (Tucker, 1951). The particular MOCNESS system from which these CTD data came is one of two net systems. The MOCNESS-1 has nine rectangular nets (1m x 1.4 m) which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe et al., 1976). The MOCNESS-10 (with 10 m2 nets)carries 6 nets of 3.0-mm circular mesh. In both systems, &#039;the underwater unit sends a data frame, comprised of temperature, depth, conductivity, net-frame angle, flow count, time, number of open net, and net opening/closing, to the deck unit in a compressed hexadecimal format every 2 seconds and from the deck unit to a microcomputer every 4 seconds... Temperature (to approximately 0.01 deg C) and conductivity are measured with SEABIRD sensors. Normally, a modified T.S.K.-flowmeter is used... Both the temperature and conductivity sensors and the flow meter are mounted on top of the frame so that they face horizontally when the frame is at a towing angle of 45deg... Calculations of salinity (to approximately 0.01 o/oo S), potential temperature (theta), potential density (sigma), the oblique and vertical velocities of the net, and the approximate volume filtered by each net are made after each string of data has been received by the computer.&#039; (Wiebe et al., 1985) In addition, data were collected from four other sensors attached to the frame: the Transmissometer, the Fluorometer, the Down welling light sensor, and the Oxygen sensor. A SeaBird underwater pump was also included in the sensor suite. <p> It should be noted that due to Antarctic cold, the first few minutes of data are often of questionable value as they are extremely variable and have a high frequency of &#039;50.000&#039; (indicating &#039;bad values&#039;) in the temp, theta and sal fields. Once the sensors encounter deeper, warmer water, they start recording good values. </p> <p>For additional information, contact the <a href="/jg/serv/globec/soglobec/inventory.html0?project,name_prin"> chief scientist</a> for the cruise. 10105 zoo_moc zoo_moc http://globec.whoi.edu/jg/serv/globec/soglobec/zoo_moc.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu:80/jg/info/globec/soglobec/zoo_moc%7D? <p align="center"><b>Zooplankton abundance and biomass from MOCNESS nets using <a href="#sil">silhouette analysis<br> </a>NB Palmer, austral fall & winter of 2001 & 2002</b></p> <p>The MOCNESS-1 plankton sampler has nine rectangular nets (1m x 1.4 m) with a mesh size of 0.333 mm, which are opened and closed sequentially by commands through conducting cable from the surface (Wiebe <i>et al.</i>, 1976).</p> <p><b>Cruises:</b><br> Nathaniel B. Palmer, April-June 2001 (NBP01-03), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0103,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, July-Sept. 2001 (NBP01-04), 17 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0104,data_type%20eq%20cruise_report"> cruise report</a><br> Nathaniel B. Palmer, April-May 2002 (NBP02-02), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0202,data_type%20eq%20cruise_report"> cruise report</a> <br> Nathaniel B. Palmer, July-Sept. 2002 (NBP02-04), 19 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory}?project%20eq%20NBP0204,data_type%20eq%20cruise_report"> cruise report</a></p> <p align=center>This is a graph of the vertical distribution of biomass from the Winter 2001 Cruise, NBP0103:</p> <p align=center><img src="http://globec.whoi.edu/globec-dir/data_doc/nbp0103zoosm2.png" width="622" height="324"></p> <br> <br> <br> <p align=center>This is a graph of the vertical distribution of biomass from the Winter 2001 Cruise, NBP0104:</p> <p align=center><img src="http://globec.whoi.edu/globec-dir/data_doc/nbp0104zoosm.png" width="625" height="323"></p> <br> <h3 align=center>MOCNESS Sample Analysis<br> (From Ashjian et al., 2004)</h3> <p>Biomass (wet weight) and abundance were determined principally by silhouette digitization of taxa lengths and conversion to equivalent wet weights according to the equations and methods adapted from Davis and Wiebe (1985) and Wiebe et al. (2004). New formulas were calculated for Southern Ocean krill because the length-weight relationship (Wet Weight = 0.0054*Length^3.214) differed from that of the North Atlantic euphausiids (Wet Weight = 0.0138*Length^3.071; Davis and Wiebe, 1985).<a name="sil"></a></p> <p>Silhouette photographs first were obtained from each sample; this photograph then was scanned with an Epson Expression 1600 scanner at 1200 dpi to produce a Tagged Image File Format (TIF) image. Identification and measurement of organisms from the tiff image were accomplished manually using the specialized MATLABæ (Mathworks, Inc.) routine, the WHOI Silhouette <a href="http://globec.whoi.edu/software/digi_prog/WHOI_Silhouette_DIGITIZER.htm">DIGITIZER</a> (v 1.0) (Little and Copley, 2003). A scanned photographic image of an aliquot of a sample was displayed with a superimposed reference grid on the computer screen. The operator identified each organism to taxonomic and/or size category by selecting the appropriate category button. Organism lengths (both straight and curved) then were measured by the operator using the cursor on the computer screen. Although the nominal resolution of the measurement is 0.02 mm, in practice the resolution was ~0.05 mm. In instances where there were too many organisms of a given type to justify measuring every individual organism, the DIGITIZER routine generated a list of randomly located cells to systematically sub-sample the overall image. Each organism's biomass was calculated automatically from its length measurement using the appropriate length-weight relationship.</p> <p><b>References:</b> <p>Ashjian, C.J, Rosenwaks, G.A., Wiebe, P.H., Davis, C.S., Gallager, S.M., Copley, N.J., Lawson, G.L., Alatalo, P. 2004. Distribution of Zooplankton on the Continental Shelf of Marguerite Bay, Antarctic Peninsula, during Austral Fall and Winter, 2001. Deep-Sea Research II <b>51(17-19)</b>: 2073-2098.</p> <p>Davis, C.S., Wiebe, P.H., 1985. Macrozooplankton biomass in a warm-core Gulf Stream ring: Time series changes in size structure, taxonomic composition, and vertical distribution. Journal of Geophysical Research <b>90</b>, 8871-8882.</p> <p>Little. W.S., Copley, N.J. 2003. WHOI Silhouette Digitizer version 1.0 User's Guide. Woods Hole Oceanographic Institution Technical Report #2003-05, 63 pp.</p> <p>Wiebe, P.H., K.H. Burt, S. H. Boyd, A.W. Morton, 1976. The multiple opening/closing net and environmental sensing system for sampling zooplankton. Journal of Marine Research, <b>34(3)</b>: 313-326.</p> <p>Wiebe, P.H., C. J. Ashjian, S. M. Gallager, C. S. Davis, G. L. Lawson, and N. J. Copley. 2004. Using a high powered strobe light to increase the catch of Antarctic krill. Marine Biology. <b>144(3)</b>: 493 - 502.</p> <hr> <p align=center> <img src="http://globec.whoi.edu/globec-dir/data_doc/newmocmapsm2.jpg" width="587" height="314"><br> <b>Figure 1. Map of Tow locations, Fall and Winter, 2001</b></p> <br> <br> <p align=center><b>Table 1.</b> Summary of locations, times, and depths for the twelve net tows.<br> (<b>Note:</b> Winter tows 14 and 15 were considered one tow because when ice and malfunction led to no data in the top three nets of Tow 14, MOC Tow 15 was fished in the upper 90 meters to compensate.)</p> <table border=1> <tr><th>Cruise</th><th>Region</th><th>Tow <br>Number</th><th>Date </th><th>Time<br>(Local)</th><th>Light* </th><th> Lat(°S)</th><th> Lon(°W)</th><th>Tow Depth(m)</th><th>Bottom Depth(m)</th><th>Ice Cover<br>(tenths)</th></tr> <tr><td>Fall</td><td>Offshore </td><td> 6 </td><td>05/04/01 </td><td> 1332 </td><td> D </td><td> 66° 40.17 </td><td> 73° 22.08 </td><td> 0-1001 </td><td> 3650</td><td> 0</td></tr> <tr><td> </td><td>Midshelf 1 </td><td>1 </td><td> 04/30/01</td><td> 2050 </td><td> N </td><td> 66° 10.80 </td><td> 69° 10.47 </td><td> 0-306 </td><td>360 </td><td> 0</td></tr> <tr><td> </td><td> Midshelf 2 </td><td>3 </td><td>05/02/01 </td><td> 0320 </td><td>N </td><td> 66° 48.53 </td><td> 70° 21.42</td><td> 0-348 </td><td> 600 </td><td> 0</td></tr> <tr><td> </td><td>Midshelf 3 </td><td>12 </td><td> 05/13/01 </td><td>1830 </td><td> N</td><td>68° 23.62</td><td> 72° 18.44 </td><td> 0-356 </td><td>400 </td><td> 0</td></tr> <tr><td> </td><td>Midshelf 4 </td><td>16 </td><td> 05/18/01</td><td> 0854 </td><td>N </td><td> 68° 59.43</td><td> 74° 55.77 </td><td> 0-340 </td><td> 350 </td><td> 0</td></tr> <tr><td> </td><td>Marguerite Bay </td><td>24 </td><td> 05/29/01</td><td> 0300 </td><td> N </td><td> 67° 55.33 </td><td> 68° 30.69 </td><td> 0-602 </td><td>690 </td><td> 0</td></tr> <tr><td>Winter </td><td> Offshore </td><td> 11 </td><td> 08/11/01 </td><td> 0918 </td><td>T </td><td> 67° 14.69 </td><td> 74° 25.27 </td><td> 0-989 </td><td>2917 </td><td>10</td></tr> <tr><td> </td><td> Midshelf 1 </td><td> 17</td><td>08/26/01 </td><td>0306 </td><td> N </td><td> 66° 11.13 </td><td> 69° 06.21 </td><td> 7-305 </td><td> 346 </td><td> 6</td></tr> <tr><td> </td><td> Midshelf 2 </td><td> 4 </td><td> 07/31/01</td><td>0949 </td><td> D </td><td> 66° 45.18 </td><td> 70° 09.64 </td><td> 11-413 </td><td>501 </td><td> 8</td></tr> <tr><td> </td><td> Midshelf 3 </td><td>13 </td><td> 08/17/01</td><td>2117 </td><td>N </td><td>68° 13.21</td><td> 72° 56.53 </td><td> 0-230 </td><td> 325 </td><td> 10</td></tr> <tr><td> </td><td> Midshelf 4 </td><td>14 </td><td> 08/21/01 </td><td> 1136 </td><td>D </td><td> 69° 15.55 </td><td> 75° 34.00 </td><td> 20-290 </td><td> ~340 </td><td>7</td></tr> <tr><td> </td> <i><td> </td></i><td> 15 </td><td> 08/22/01 </td><td> 0327 </td><td> N </td><td> 69° 12.30 </td><td> 75° 43.90 </td><td> 0-91 </td><td> ~350 </td><td> 9</td></tr> <tr><td> </td><td> Marguerite Bay </td><td>9 </td><td>08/08/01 </td><td> 0215 </td><td> N </td><td> 67° 53.74</td><td> 68° 10.82 </td><td> 0-488 </td><td> 600+ </td><td> 9</td></tr> </table> <p><b>*</b>Light conditions are designated as:<br> "D" = day, sunlight present; <br> "N" = night, darkness;<br> "T" = twilight</p> <p> <b>See companion data sets:<br> </b> 1. <a href ="http://globec.whoi.edu/jg/serv/globec/soglobec/mocness_biovols_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/mocness_biovols%7D"> Zooplankton biovolume values from MOCNESS tows</a> - this data set is derived from displacement volume measurements and dry weight conversion calculations from the same set of samples as the above data.<br> 2. <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/zooabund_nbp.html0{dir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/zooabund_nbp}">Zooplankton Abundance Based on Taxa and Life Stages or Size</a> - these abundance values on the same tows were derived by counting and identifying a subset of the zooplankton to the species and life stage for euphausiids and dominant copepods and to taxonomic group with broad size categories for other zooplankton (pteropod, chaetognath, polychaete, etc.).<i> <hr> </i> <p>For Information, contact:<br> Carin Ashjian<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br> 508-289-3457 (ph) 508-457-2169 (fax)<br> cashjian@whoi.edu<br> <a href="http://www.whoi.edu/science/B/people/cashjian/index.html">http://www.whoi.edu/science/B/people/cashjian/index.html<br> </a> <b>-or-</b><br> Nancy Copley<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br> 508-289-3204 (ph) 508-457-2169 (fax)<br> ncopley@whoi.edu</p> <p> <i>last updated 08/15/06</i> Biomass (wet weight) and abundance were determined principally by silhouette digitization of taxa lengths and conversion to equivalent wet weights according to the equations and methods adapted from Davis and Wiebe (1985) and Wiebe et al. (2004). New formulas were calculated for Southern Ocean krill because the length-weight relationship (Wet Weight = 0.0054*Length^3.214) differed from that of the North Atlantic euphausiids (Wet Weight = 0.0138*Length^3.071; Davis and Wiebe, 1985). Silhouette photographs first were obtained from each sample; this photograph then was scanned with an Epson Expression 1600 scanner at 1200 dpi to produce a Tagged Image File Format (TIF) image. Identification and measurement of organisms from the tiff image were accomplished manually using the specialized MATLABæ (Mathworks, Inc.) routine, the WHOI Silhouette <a href="http://globec.whoi.edu/software/digi_prog/WHOI_Silhouette_DIGITIZER.htm">DIGITIZER</a> (v 1.0) (Little and Copley, 2003). A scanned photographic image of an aliquot of a sample was displayed with a superimposed reference grid on the computer screen. The operator identified each organism to taxonomic and/or size category by selecting the appropriate category button. Organism lengths (both straight and curved) then were measured by the operator using the cursor on the computer screen. Although the nominal resolution of the measurement is 0.02 mm, in practice the resolution was ~0.05 mm. In instances where there were too many organisms of a given type to justify measuring every individual organism, the DIGITIZER routine generated a list of randomly located cells to systematically sub-sample the overall image. Each organism&#039;s biomass was calculated automatically from its length measurement using the appropriate length-weight relationship. <p> Nathaniel B. Palmer, April-June 2001 (NBP01-03), 24 tows, <a href="http://globec.whoi.edu/jg/serv/globec/soglobec/inventory.html2%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/inventory%7D?project%20eq%20NBP0103,data_type%20eq%20cruise_report"> cruise report</a> 10106 alongtrack alongtrack http://jgof.wh.whoi.edu/jg/serv/globec/gb/brdscale/al_shipdata.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/alongtrack%7D <h2 align=center> R/V Albatross Globec broadscale cruises 1995-1999,<br> shipboard meteorology and sea surface measurements<br> along the ship's track</h2> <p> <b> Comments submitted by Jim Manning</b> <p> <ol> <li> These data are accessed under the GLOBEC<br> homepage-->Georges Bank data-->broadscale-->alongtrack &nbsp; <b>or</b> <br> homepage-->Georges Bank data-->broadscale-->{year}-->alongtrack &nbsp; <b>or</b> <br> homepage-->Georges Bank data-->process-->alongtrack &nbsp; <b>or</b><br> homepage-->Georges Bank data-->process-->{year}-->alongtrack. </p> <p> <li> These are single ascii files per cruise with several variables merged to one minute (interpolated) time steps. The user should be aware of the availability of the unmerged "raw" data if they want the actual data which, for some sensors/variables, was recorded as frequent as every 5 seconds and by more than one instrument. Contact Jim Manning for access to thes data. </p> <p> <li> The first column is the time stamp which, for Albatross convention, is "yrday1_local" which means, for example, that a time of "1.5" represents local noontime on Jan 1st. Note that the "Albatross yearday convention changed to GMT after year 2000, so the user must pay attention to the time stamp in future cruises. </p> <p> <li> I have been processing Albatross and Delaware alongtrack data on an "as requested" basis so just let me know when you want a particular cruise that is not already posted. More recent (post GLOBEC) data are being stored in as ORACLE database and served via OpenDAP as documented <A href="http://www.nefsc.noaa.gov/epd/ocean/MainPage/AlongTrack.html">elsewhere.</A> </p> <p> <li> We all understand this data (shipboard temp, salt, wind, etc.) should be treated as uncalibrated records and <b>should not be used for other than exploratory purposes</b>. </p> </ol> <pre> <b>Any questions, contact:</b> Jim Manning National Marine Fisheries Service Woods Hole, Ma 02543 voice: 508 495 2211 fax: 508 495 2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> <i>Updated 09/15/05; gfh w/ input from J.Manning</i> </pre> </pre> These are single ascii files per cruise with several variables merged to one minute (interpolated) time steps. The user should be aware of the availability of the unmerged &#039;raw&#039; data if they want the actual data which, for some sensors/variables, was recorded as frequent as every 5 seconds and by more than one instrument. 10107 bongovols bongovols http://globec.whoi.edu/jg/serv/globec/gb/broadscale/bongovols.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/bongovols%7D <hr> <h4 align=center> BioVolume Data from Bongo Tows during Broadscale Cruises, 1995-1999<br> Dave Mountain, Jack Green and Joe Kane, NMFS </h4> <p> This displacement volume data comes from one net with a mesh size of 333 um.</p> <p> <table width=80% align=center> <tr align=left> <th> column header</th> <th> meaning </th> <th> units</th> </tr> <tr align=left> <td>raw_vol</td> <td> raw volume</td> <td>cc</td></tr> <tr align=left> <td>displ_vol</td> <td>displacement volume</td> <td>cc/100m3</td></tr> <tr align=left> <td>haul_factor</td> <td>haul factor</td> <td>100/volume filtered (m3)</td></tr> </table> </p> displacement volume is a normalized displacement volume and is calculated: <b>raw_vol * haul_factor</b> This displacement volume data comes from one net with a mesh size of 333 um. <table align="center" width="80%"> <tbody><tr align="left"><th> column header</th> <th> meaning </th> <th> units</th> </tr> <tr align="left"> <td>raw_vol</td> <td> raw volume</td> <td>cc</td></tr> <tr align="left"> <td>displ_vol</td> <td>displacement volume</td> <td>cc/100m3</td></tr> <tr align="left"> <td>haul_factor</td> <td>haul factor</td> <td>100/volume filtered (m3)</td></tr> </tbody></table> displacement volume is a normalized displacement volume and is calculated: <b>raw_vol * haul_factor</b> 10109 cp_decibels cp_decibels http://globec.whoi.edu/jg/serv/globec/gb/broadscale/1998/cp_decibels.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/cp_decibels%7D Could not find either xml or text based metadata file for object cp_decibels 10110 cp_depths cp_depths http://globec.whoi.edu/jg/serv/globec/gb/broadscale/1998/cp_depths.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/cp_depths%7D Could not find either xml or text based metadata file for object cp_depths 10111 cp_lat_lon cp_lat_lon http://globec.whoi.edu/jg/serv/globec/gb/broadscale/1998/cp_lat_lon.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/cp_lat_lon%7D Could not find either xml or text based metadata file for object cp_lat_lon 10112 ctd_hydrography ctd_hydrography http://globec.whoi.edu/jg/serv/globec/gb/broadscale/ctd_hydrography.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/ctd_hydrography%7D <h2 align=center> Broad-scale Hydrography, 1995 - 1999</h2> <p> <pre> <b>If you encounter any questionable values or have other questions, contact:</b> David Mountain National Marine Fisheries Servce, NEFC Woods Hole, MA 02540 voice: 508 495 2000 fax: 508 495 2258 email: <a href="mailto:David.Mountain@noaa.gov">David.Mountain@noaa.gov</a> </pre> <p> <h2 align=center>File Descriptions:</h2> <p> At level 1 in the comments field, the user has three options for selecting CTD profile data available from this cruise: <p> mark5CTD link - Links the user to the Neil Brown Mark-5 CTD profiles. The Mark-5 profiler, has a higher sampling rate then the SeaBird SEACAT, was instrumented with an expanded suite of sensors and deployed almost exclusively at GLOBEC Standard stations. <p> seabirdCTD link - Links the user to the SeaBird SEACAT profiler deployed with the bongo plankton net tow system at Standard and Intermediate stations. The upcast portion of the tow is the most reliable and that is what is reported here. These profiles do not contain the parameters: light transmission, fluorescence, and scalar par. Users working with the plankton data may want to work with this data set exclusively. <p> primary link - Links the user to the best hydrography coverage available for the cruise. The "primary version", in most cases, is a composite of both the Mark-5 and SEACAT CTD casts. These casts have been extracted from their respective cruise files and sorted by time. As a result, the reported cast and station numbers are frequently duplicated and random in order. When present, SeaBird profiles are identified with a one hundred series cast number to distinguish from a Mark-5 profile, however, this convention is inconsistent and does not always appear in all cruises (primary link only). <p> <h2 align=center>Procedure for processing primary CTD data </h2> The following is an outline of the methods used to process the "primary" CTD data from the 1995 Broad scale surveys. <ol> <li>Upon completion of each broad scale cruise, preliminary processing of the MK5 data was carried out: <ol> <li><b>"first differencing"</b> (called from within CTDPOST) of the Raw cast files was completed. This program flags any data where the difference between sequential scans exceed some preset limit. </li> <p> <li><b>"smart editor"</b> used to interpolate over any flagged values from "first differencing"</li><p> <li><b>ENDCAST XXX</b> (a dos batch routine where xxx=cast#) runs MK5PROC.EXE which creates pressure averaged, pressure centered 1 db files (.PRE files). These routines (pressure averaging and pressure centering) were developed by Bob Millard at WHOI and were modified for the Mk5. "ENDCAST" also updates a cruise header file, and backs up the data to floppy) </li><p> <li><b>CTDPLOT</b> (visual basic program by David Mountain) was run at each station to plot out the cast profile and to visually inspect the data.</li><p> <li><b>MK5BOT.EXE</b> This routine (again, developed by Bob Millard) extracts and averages 30 data scans around the data scan number (as identified in the cast .BTL file) at which bottles were fired during a cast and appends to a cruise bottle file. These files were reviewed after each cruise to ensure that each btl fired had a corresponding observation record in the btl file. If we forgot to record a btl fired (forgot to press [CTRL] F3), we used an observation from the .PRE files.</li><p> </ol> <li>Salinity samples (btm) collected on each cruise were analyzed on a guildline autosal <ul> <li><b>tstslt.bas</b> was used to compare the cruise btl file with the autosal output file</li> <li><b>mk5xxxx.m</b> (where xxxx=4 digit cruise id) was used to calculate the mean conductivity offset</li> </ul> <p> <ol> <li>any single comparison that was greater than -0.1 or +0.1 was ignored.</li> <li>the mean offset and standard deviation (std) were calculated</li> <li>any single comparison that was greater than +/- 2 std's was discarded as an outlier</li> <li>the mean and std were re-calculated</li> <li>The offset series for each cruise were inspected to insure that a time dependant trend was not evident and that using a mean offset was appropriate.</li><p> </ol> <p> <li>The mean conductivity offsets were applied to each cruise data set using <b>MK5final.bas</b>. <b>MK5cru.fin</b> was read in as input containing the necessary information for cruise id, directory, and most importantly conductivity offset. The output was pressure averaged, pressure centerred .PRS files. <p><ul> <li>During EN261 and ALB9506, seabird data was used to supplement for primary hydro data when there were problems with the MK5 (or winch). Seabird CTD data were processed to pressure averaged, 1 db files using the manufacturer's software <b>DATCNV, ALIGNCTD, BINAVG, DERIVE,</b> and <b>ASCIIOUT</b>. When Seabird data were used as "primary" data, the casts were numbered >100. The same steps outlined in 2a)--2e) were followed in the quality controlling of the seabird salinity data except that the comparison was done with salinity (rather than conductivity). The seabird cast data have also been processed to NODC formatted files and are available in this format in a NEFSC anonymous ftp account ftp: ftp/pub/hydro.</li> </ul><p> <li>Final data checking was accomplished with a matlab program called <b>dchkXX.m</b> (where xx is the cruise code) that did the following: <p> <ol> <li>read in the cruise .h3 file (output of <b>ENDCRUIS.FOR</b>) and calculated the distance and time between consecutive casts and wrote the results to headchk.xx (where xx is the cruise code). Any speed that was >= 10 knots was verified with the original cruise logs and if found in error, was corrected.</li></P> <li>read in the cast files and went through a series of allowable "range checking" of T, S, Sigma-t, and fluorescence. Profiles of these 4 parameters are plotted to the screen for visual inspection.<p> <pre> RANGES 0 <--- T ---> 25 30 <--- S ---> 37 0 <--- Fl ---> 5 -0.05 <--- ST---> 0.1 </pre> The above flagged values were written out to <b>datachk.xx</b> <p> </ol></li> </ol> <p> ** note: in most instances, the positive sigma-t differences were O.K. and occurred when stratification had developed or when the MK5 sampled through strong gradients like the shelf / slope front. However, there were cases of "hysteresis" (sp?) when the MK5 or seabird sampled through sharp t/s gradients. In these instances, I had to delete the records.<p> <p> ** On a number of occasions, there were negative fluorescence values for the sfc observation. (These were also observed in the raw data...A consultant with Sea-tech said that this is probably "noise" associated with its equilibrating when just powered up). For these casts, I looked in the raw data files, and chose a substitute fluorescence value.<p> <p> The output listing of the flagged observations from "datachk.m" are kept on file (and can be made available). Any record deletions are noted. <p> <i>Prepared by: Maureen Taylor, NMFS/Woods Hole, 2/7/1996<br> last updated: 19 Nov. 2004; gfh </i> </pre> <ul> <li>The Mark-5 profiler, has a higher sampling rate then the SeaBird SEACAT, was instrumented with an expanded suite of sensors and deployed almost exclusively at GLOBEC Standard stations. <li>SeaBird SEACAT profiler deployed with the bongo plankton net tow system at Standard and Intermediate stations. The upcast portion of the tow is the most reliable and that is what is reported here. These profiles do not contain the parameters: light transmission, fluorescence, and scalar par. The primary version, in most cases, is a composite of both the Mark-5 and <li>SEACAT CTD casts. These casts have been extracted from their respective cruise files and sorted by time. As a result, the reported cast and station numbers are frequently duplicated and random in order. When present, SeaBird profiles are identified with a one hundred series cast number to distinguish from a Mark-5 profile, however, this convention is inconsistent and does not always appear in all cruises (primary link only). </ul> The following is an outline of the methods used to process the "primary" CTD data from the 1995 Broad scale surveys. <ol> <li>Upon completion of each broad scale cruise, preliminary processing of the MK5 data was carried out: <ol> <li><b>"first differencing"</b> (called from within CTDPOST) of the Raw cast files was completed. This program flags any data where the difference between sequential scans exceed some preset limit. </li> <p> </p><li><b>"smart editor"</b> used to interpolate over any flagged values from "first differencing"</li><p> </p><li><b>ENDCAST XXX</b> (a dos batch routine where xxx=cast#) runs MK5PROC.EXE which creates pressure averaged, pressure centered 1 db files (.PRE files). These routines (pressure averaging and pressure centering) were developed by Bob Millard at WHOI and were modified for the Mk5. "ENDCAST" also updates a cruise header file, and backs up the data to floppy) </li><p> </p><li><b>CTDPLOT</b> (visual basic program by David Mountain) was run at each station to plot out the cast profile and to visually inspect the data.</li><p> </p><li><b>MK5BOT.EXE</b> This routine (again, developed by Bob Millard) extracts and averages 30 data scans around the data scan number (as identified in the cast .BTL file) at which bottles were fired during a cast and appends to a cruise bottle file. These files were reviewed after each cruise to ensure that each btl fired had a corresponding observation record in the btl file. If we forgot to record a btl fired (forgot to press [CTRL] F3), we used an observation from the .PRE files.</li><p> </p></ol> </li><li>Salinity samples (btm) collected on each cruise were analyzed on a guildline autosal <ul> <li><b>tstslt.bas</b> was used to compare the cruise btl file with the autosal output file</li> <li><b>mk5xxxx.m</b> (where xxxx=4 digit cruise id) was used to calculate the mean conductivity offset</li> </ul> <p> </p><ol> <li>any single comparison that was greater than -0.1 or +0.1 was ignored.</li> <li>the mean offset and standard deviation (std) were calculated</li> <li>any single comparison that was greater than +/- 2 std&#039;s was discarded as an outlier</li> <li>the mean and std were re-calculated</li> <li>The offset series for each cruise were inspected to insure that a time dependant trend was not evident and that using a mean offset was appropriate.</li><p> </p></ol> <p> </p></li><li>The mean conductivity offsets were applied to each cruise data set using <b>MK5final.bas</b>. <b>MK5cru.fin</b> was read in as input containing the necessary information for cruise id, directory, and most importantly conductivity offset. The output was pressure averaged, pressure centerred .PRS files. <p></p><ul> <li>During EN261 and ALB9506, seabird data was used to supplement for primary hydro data when there were problems with the MK5 (or winch). Seabird CTD data were processed to pressure averaged, 1 db files using the manufacturer&#039;s software <b>DATCNV, ALIGNCTD, BINAVG, DERIVE,</b> and <b>ASCIIOUT</b>. When Seabird data were used as "primary" data, the casts were numbered >100. The same steps outlined in 2a)--2e) were followed in the quality controlling of the seabird salinity data except that the comparison was done with salinity (rather than conductivity). The seabird cast data have also been processed to NODC formatted files and are available in this format in a NEFSC anonymous ftp account ftp: ftp/pub/hydro.</li> </ul><p> </p></li><li>Final data checking was accomplished with a matlab program called <b>dchkXX.m</b> (where xx is the cruise code) that did the following: <p> </p><ol> <li>read in the cruise .h3 file (output of <b>ENDCRUIS.FOR</b>) and calculated the distance and time between consecutive casts and wrote the results to headchk.xx (where xx is the cruise code). Any speed that was >= 10 knots was verified with the original cruise logs and if found in error, was corrected.</li><p></p> <li>read in the cast files and went through a series of allowable "range checking" of T, S, Sigma-t, and fluorescence. Profiles of these 4 parameters are plotted to the screen for visual inspection.<p> </p><pre> RANGES 0 <--- T ---> 25 30 <--- S ---> 37 0 <--- Fl ---> 5 -0.05 <--- ST---> 0.1 </pre> The above flagged values were written out to <b>datachk.xx</b> <p> </p></li></ol></li> </ol> <p> ** note: in most instances, the positive sigma-t differences were O.K. and occurred when stratification had developed or when the MK5 sampled through strong gradients like the shelf / slope front. However, there were cases of "hysteresis" (sp?) when the MK5 or seabird sampled through sharp t/s gradients. In these instances, I had to delete the records.</p><p> </p><p> ** On a number of occasions, there were negative fluorescence values for the sfc observation. (These were also observed in the raw data...A consultant with Sea-tech said that this is probably "noise" associated with its equilibrating when just powered up). For these casts, I looked in the raw data files, and chose a substitute fluorescence value.</p> 10114 curtain_plot curtain_plot http://globec.whoi.edu/jg/serv/globec/gb/broadscale/1994/curtain_plot.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/curtain_plot%7D This is a 3D curtain plot of volume back scattering along the ALBATROSS IV 9404, June 1994, cruise track line. It is a 780nm visualization. For further information, contact Peter Wiebe, Woods Hole Oceanographic Institution. This is a 3D curtain plot of volume back scattering along the ALBATROSS IV 9404, June 1994, cruise track line. It is a 780nm visualization. 10115 delta_O_18 delta_O_18 http://globec.whoi.edu/jg/serv/globec/gb/broadscale/delta_O_18.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/delta_O_18%7D <h2 align=center>Oxygen Isotope data, GLOBEC and Canadian Cruises 1994-1998</h2> <p> <P>Oxygen isotope data are derived from water samples collected on GLOBEC broad-scale and contemporaneous Canadian cruises 1994-1998. The isotope ratio H<SUB>2</SUB><SUP>18</SUP>O/H<SUB>2</SUB><SUP>16</SUP>O is measured, using a VG Prism II mass-spectrometer operated by Rick Mortlock and maintained by Rick Fairbanks at LDEO, and presented in delta<SUP>18</SUP>O notation where:</P> <ul> <P><li>Replicates of each water sample are analyzed. The data presented is the average of the replicates and their difference. If the difference exceeds 0.066 the analysis is repeated. The average standard deviation of the data is 0.033.</P> <P><li>The content of the data file varies according to source, degree of editing, and some arbitrary formating changes. For broad-scale data the cruise is always given in the file name and sometimes the header. The station number is the broad-scale standard station with associated lat., long., and bottom depth. Temperature, salinity, bottle depth, and sometimes fluorescence and transmissivity data are copied from the broad-scale hydrographic data file.</P> <P><li>Canadian data are from C.S.S. Parizeau cruises. The station and bottle number are unique to a particular cruise. When depth is listed as pressure it is numerically equivalent to depth in meters. Hydrographic data are supplied by Gary Bugden at the Bedford Institute of Oceanography.</P> <P><li>The time for each file is denoted by month and year. More precise day and hour information is available in the original hydrographic file.</P> </ul> <pre> <b>Contributors:</b> Bob Houghton and Rick Fairbanks <b>Any questions, contact:</b> Bob Houghton Lamont-Doherty Earth Observatory of Columbia University Palisades, NY 10964 voice: 845 365 8328 fax: 845 365 8157 email: <a href="mailto:houghton@ldeo.columbia.edu">houghton@ldeo.columbia.edu</a> <i>Updated: November 15, 2004; gfh</i> </pre> Oxygen isotope data are derived from water samples collected on GLOBEC broad-scale and contemporaneous Canadian cruises 1994-1998. The isotope ratio H218O/H216O is measured, using a VG Prism II mass-spectrometer operated by Rick Mortlock and maintained by Rick Fairbanks at LDEO. <ul> <li> Replicates of each water sample are analyzed. The data presented is the average of the replicates and their difference. If the difference exceeds 0.066 the analysis is repeated. The average standard deviation of the data is 0.033. <li> The content of the data file varies according to source, degree of editing, and some arbitrary formating changes. For broad-scale data the cruise is always given in the file name and sometimes the header. The station number is the broad-scale standard station with associated lat., long., and bottom depth. Temperature, salinity, bottle depth, and sometimes fluorescence and transmissivity data are copied from the broad-scale hydrographic data file. <li> Canadian data are from C.S.S. Parizeau cruises. The station and bottle number are unique to a particular cruise. When depth is listed as pressure it is numerically equivalent to depth in meters. Hydrographic data are supplied by Gary Bugden at the Bedford Institute of Oceanography. <li> The time for each file is denoted by month and year. More precise day and hour information is available in the original hydrographic file. </ul> 10118 vbs vbs http://globec.whoi.edu/jg/serv/globec/gb/broadscale/vbs.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/broadscale/,info=globec.whoi.edu/jg/info/globec/gb/broadscale/vbs%7D <h3 align=center> Volume back scattering, Albatross IV 9205 and 9607</h3> <p> The data are reported at 20 depth intervals (1-20meters) per yearday and position over a given track line. </p> <i>last updated January 7, 2009</i> The data are reported at 20 depth intervals (1-20meters) per yearday and position over a given track line. Uses the vbs method, similar in function to the def method. 10119 2dmodel_m2only 2dmodel_m2only http://globec.whoi.edu/jg/serv/globec/gb/modeling/2dmodel_m2only.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/modeling/,info=globec.whoi.edu/jg/info/globec/gb/modeling/2dmodel_m2only%7D <H2 align=center> A 2D Model of Georges Bank in the Summer, Forced Only By M2 Tides </H2> <h4 align=center>Contact: J. Pringle <br>pringle@poto.ucsd.edu</h4> This 2D model of Georges Bank was developed by Dr. Changsheng Chen of the University of Georgia, and has been described in <I>Chen et al. (1995), Chen and Beardsley (1995), </I>and <I>Franks and Chen (1996).</I>&nbsp;&nbsp;&nbsp; It is based on the Ecom-si code described in <I>Blumberg and Mellor (1987)</I>.&nbsp; It is run with a uniform summertime stratification of 0.03 degrees Celsius per meter, and, in the movies below, has been forced with the M2 tides and run until the density field has reached a steady state (averaged over a tidal cycle).&nbsp; The model has 61 levels in the vertical, and has 1 km horizontal resolution.&nbsp;&nbsp; The vertical turbulence closure is a full level 2.5 Mellor Yamada scheme. <P>The particle tracking code used to produce the movies below were written by J. Pringle based on routines kindly provided by Changsheng Chen. <H3> Playing the movies below:</H3> <P>The movies below are in the .flc format- <A HREF="http://crusty.er.usgs.gov/flc.html">Instruction for playing these movies </A>can be found on Rich Signell's web page.&nbsp;&nbsp; <H3> If your link to the Internet is slow:</H3> All of the movies and this page can be downloaded as a <A HREF="ftp://globec.whoi.edu/pub/jpringle/movies.tar.gz">compressed tar file</A> for those with slow links- this is much faster since the combined tar file is one-third the size of the files individually. <BR>&nbsp; <H2> Movies of the Flow, Temperature, and Vertical Mixing Fields</H2> <BLOCKQUOTE>The flow, temperature, and vertical mixing coefficients for temperature are shown below for four portions of the model domain: <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/pofeildtop.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_pofeildtop.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Georges Bank Crest</FONT></A>- Note the tidally modulated vertical mixing, and the vertical phase lags in the velocity fields caused by friction.&nbsp;&nbsp; These interact with the horizontal density gradients to create unstable stratification on the bank for part of each tidal cycle. [6.4Mbytes] <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/pofeildnb.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_pofeildnb.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Northern Flank</FONT></A>- Note the strong vertical phase shifts in the cross bank velocity over the steepest part of the bank- These are driven by intense horizontal pressure gradients formed when less dense water is pulled off the bank by tides.&nbsp;&nbsp; These phase shifted currents lead to unstable stratification and strong vertical mixing over the steepest portions of the north flank.&nbsp; [The line contours in the plots of vertical diffusivity represent diffusivities of 0.25, 0.5 and 0.75 meters squared per second]. [3.8MBytes] <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/pofeildiw.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_pofeildiw.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Northern Flank, extended</FONT></A>- Same as the above movie, but the region displayed has been shifted 35 km northward to better illustrate the generation of internal tides. [3.8Mbytes] <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/pofeildsb.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_pofeildsb.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Southern Flank</A>- </FONT>Again, notice the internal tide generation and frictional and buoyancy driven vertical phase lags in the velocity fields and the tidally modulated mixing. [2.7Mbytes] <BR>&nbsp; <BR>&nbsp; </BLOCKQUOTE> <H2> Movies of Float paths</H2> <BLOCKQUOTE>The movies below show the paths of particles released in several columns over the bank. The floats are moved both by the mean currents and the turbulent velocities which are parameterized in the model by vertical diffusivities. &nbsp;&nbsp; The movies run for two tidal cycles. <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/coloumntop.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_coloumntop.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Georges Bank Crest</FONT></A>- Notice the horizontal dispersion of the particles caused by vertical mixing and horizontal shear flows.&nbsp; This leads to an effective horizontal diffusivity of 40-80 meters squared per second.&nbsp; [29Mbytes] <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/coloumnnb.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_coloumnnb.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Northern Flank</FONT></A>- Notice the cross-bank transport of particles in the bottom boundary layer over the steepest portion of the bank (<I>Chen and Beardsley</I>, In Press), and the shear/strain dispersion elsewhere in the bottom boundary layer.&nbsp; Also notice the lack of a net motion over a tidal cycle of particles in the well stratified regions. [29.3Mbytes] <BR>&nbsp; <P><A HREF="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/coloumnsb.flc"><IMG SRC="http://globec.whoi.edu/globec-dir/more/moreweb/jpringle/qrtr_coloumnsb.jpg" HEIGHT=137 WIDTH=187><FONT SIZE=+1>&nbsp; Southern Flank</FONT></A>-&nbsp; Note the difference in the horizontal dispersion of the particles in and out of the bottom boundary layers- The presence of vertical stratification inhibits vertical mixing and thus inhibits the shear/strain horizontal diffusion mechanism.&nbsp;&nbsp; Also notice the lack of any mean cross bank motion of particles in the bottom boundary layer. [8.7Mbytes] <BR>&nbsp;</BLOCKQUOTE> <H2> &nbsp;Bibliography:</H2> <BLOCKQUOTE>Blumberg, A.F. and G.L. Mellor. 1987.&nbsp; A Description of a Three-Dimensional Coastal Ocean Circulation Model.&nbsp; <I>Three -Dimensional Coastal Ocean Models,&nbsp; </I>N.S. Heaps, ed.&nbsp; Coast. and Estuarine Sci., 4, pp. 1-16 <P>Chen, C. and&nbsp; R.C. Beardsley. 1995. A Numerical Study of Stratified Tidal Rectification Over a Finite-Amplitude Symmetric Bank.&nbsp; J. Phys. Oceanogr., 25, pp. 2090-2110 <P>Chen, C., R.C. Beardsley., and R. Limeburner.&nbsp; 1995. A Numerical Study of Stratified Tidal Rectification Over Georges Bank.&nbsp; J. Phys. Oceanogr., 25, pp. 2111-2128 <P>Franks, P. J. S. and C.&nbsp; Chen. 1996.&nbsp; Plankton Production in Tidal Fronts: A Model of Georges Bank in Summer.&nbsp; J. Mar. Res., 54, pp. 631-651 <BR>&nbsp;</BLOCKQUOTE> </BLOCKQUOTE> 10121 FVCOM FVCOM http://globec.whoi.edu/jg/serv/globec/gb/modeling/FVCOM.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/modeling/,info=globec.whoi.edu/jg/info/globec/gb/modeling/FVCOM%7D <p> The following is excerpted from the SMAST/CMAST website with permission from Dr. Chen:</p> <h3 align=center>"MODELING STUDIES OF THE ECOSYSTEM IN THE GULF OF MAINE/GEORGES BANK"</h3> <p>"The objective of our modeling exploration in the Gulf of Maine/Georges Bank is to understand physical and biological interactions associated with dynamics of tidal mixing fronts, local and remote wind forcings, diurnal and seasonal heat fluxes, and low-salinity water intrusions. Our particular interests are in (1) the influences of boundary-layer dynamics and stratification on temporal and spatial variations of plankton and larval fish in tidal mixing fronts; (2) impacts of large-scale winter storms, temperature, turbulence, and food on the growth and retention of larval cod and haddock; and (3) physical mechanisms responsible for the cross-frontal transports of water masses, nutrients, and phytoplanktons.</p> <p>This is a multidisciplinary project that is being conducted by collaborating with Dr. Peter Franks, Associate Professor at Scripps Institution of Oceanography and Dr. Bob Beardsley, Senior Scientist at Woods Hole Oceanographic Institution. We have successfully developed a coupled physical and biological model for the Gulf of Maine/Georges Bank. Physical model is a modified version of the Blumberg and Mellor primitive equation of estuary and coastal oceanic circulation model (called ECOM-si). Biological model is the 3-component nutrients (N), phytoplankton (P), and zooplankton (Z) model developed by Franks et al. (1986). Numerical experiments have been conducted for both 2-D and 3-D cases. The biological model is being updated by adding two species of phytoplankton and zooplanktons, respectively, three limiting nutrients, and detritus. This project is supported by NSF/NOAA US GLOBEC North Atlantic/Georges Bank Program."</p> <p> <a href="http://codfish.smast.umassd.edu/research_projects/GB/index.html">Return to FVCOM website</a> </p> 10122 pseudocal pseudocal http://globec.whoi.edu/jg/serv/globec/gb/modeling/pseudocal.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/modeling/,info=globec.whoi.edu:80/jg/info/globec/gb/modeling/pseudocal%7D? <h3>Inverse models for <i>Pseudocalanus moultoni</i> and <i>P. newmani</i> distributions on Georges Bank in 1997</h3> <p>D.J. McGillicuddy, Jr. and A. Bucklin</p> <p>Physical and biological controls on the springtime distributions of <i>Pseudocalanus moultoni</i> and <i>P. newmani</i> on Georges Bank are examined by assimilating observations into a coupled physical-biological model. Monthly snapshots of abundance are derived from U.S. GLOBEC Georges Bank broad-scale surveys during 1997. The forward problem is posed as an advection-diffusion-reaction equation for the copepod concentration. The adjoint method of data assimilation is used to invert for the biological sources and sinks implied by the observed changes in abundance between surveys and the flow during the intervening period. Based on this analysis, the two species appear to have distinct population centers in the late winter/early spring: <i>P. moultoni</i> on the northwest flank of the Bank and <i>P. newmani</i> on the Northeast Peak and the southern tip of Browns Bank. As the growing season progresses, the clockwise circulation around Georges Bank blends reproducing (but not interbreeding) animals from the two source regions, causing their distributions to overlap by early summer. The springtime evolution of Pseudocalanus distributions in this region is driven by a complex mixture of hydrodynamic transport and species-specific population dynamics, including both growth and mortality.</p> <p>The animation shows observed abundances of <i>P. moultoni</i> (top) and <i>P. newmani</i> (bottom). The moving panels between them display the inverse model results through time, with their horizontal position proportional to the dates between January and June.</p> <p>For more information see:<br> McGillicuddy, D.J. and A. Bucklin, 2002. Intermingling of two <i>Pseudocalanus</i> species on Georges Bank. <u>Journal of Marine Research</u>, <b>60</b>, 583-604.</p> 10123 crest crest http://globec.whoi.edu/jg/serv/globec/gb/mooring/crest.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/crest%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>CREST Mooring Site <br> 41 24.461 N, 67 32.538 W</h3> <p> Two deployments were made at this site. The first deployment was between Oct 28, 1994 and Jan 21, 1995. The second deployment was between Apr 2, 1995 and Sep 30, 1995. <p> During the second deployment the transmissometer record appears to decline at a steady rate during mid-record. This maybe due to biofouling, but this trend does not appear in the fluorometer. <pre> <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> <i>updated 06/14/05; gfh</i></pre> Two deployments were made at this site. The first deployment was between Oct 28, 1994 and Jan 21, 1995. The second deployment was between Apr 2, 1995 and Sep 30, 1995. During the second deployment the transmissometer record appears to decline at a steady rate during mid-record. This maybe due to biofouling, but this trend does not appear in the fluorometer. 10124 ctd_ji ctd_ji http://globec.whoi.edu/jg/serv/globec/gb/mooring/ctd_ji.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/ctd_ji%7D <h2 align=center>GLOBEC Georges Bank Long-Term Moored Array Component<br><br>Standard CTD Sections</h2> <p> <img src="http://globec.whoi.edu/images/GBank-ctd-mooring.gif" ALIGN="center" ALT="positions of CTD stations" > <h3><pre> Long Term Section Stations LT01 41 31.0 N x 67 36.0 W LT02 41 24.5 N x 67 32.5 W LT03 41 17.0 N x 67 28.5 W LT04 41 12.5 N x 67 26.5 W LT05 41 09.5 N x 67 24.5 W LT06 41 06.0 N x 67 22.5 W LT07 41 02.0 N x 67 20.8 W LT08 40 58.0 N x 67 19.0 W LT09 40 54.5 N x 67 17.0 W LT10 40 50.5 N x 67 15.0 W LT11 40 47.0 N x 67 13.0 W LT12 40 41.5 N x 67 10.5 W LT13 40 35.7 N x 67 08.0 W LT14 40 30.0 N x 67 05.0 W NE Peak Section Stations NE01 41 28.52 N x 67 12.17 W NE02 41 31.02 N x 67 05.77 W NE03 41 33.32 N x 66 57.77 W NE04 41 35.52 N x 66 50.87 W NE05 41 38.12 N x 66 43.07 W NE06 41 40.32 N x 66 35.97 W NE07 41 42.72 N x 66 28.77 W NE08 41 45.12 N x 66 21.67 W NE09 41 47.42 N x 66 14.37 W NE10 41 49.72 N x 66 06.67 W NE11 41 52.02 N x 65 58.87 W NE12 41 54.62 N x 65 51.77 W NE13 41 56.82 N x 65 44.57 W NE14 41 59.20 N x 65 37.50 W </pre></h3> <p><pre> <b>Data submitted by:</b> James Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> <i>Updated July 14, 2005, gfh</i></pre> CTD for long term mooring cruises 10126 ctd_oc333 ctd_oc333 http://globec.whoi.edu/jg/serv/globec/gb/mooring/1998/ctd_oc333.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/ctd_oc333%7D <h2>CTD Data from Mooring Cruise <u>Oceanus</u> 333</h2><p><table border=0><tr><td><B>Contributor:</B></td><td>Richard Limeburner</td></tr> <tr><td> </td> <td>Woods Hole Oceanographic Institution</td></tr> <tr><td></td> <td><a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a></td></tr> </table> </p><p><i>updated; October 12, 2004; G.Heimerdinger</i></p></pre> CTD Data from Mooring Cruise Oceanus 333. 10127 ctd_ps ctd_ps http://globec.whoi.edu/jg/serv/globec/gb/mooring/ctd_ps.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/ctd_ps%7D <h2 align=center>CTD Data from Eastern Gulf of Maine/Scotian Shelf</h2> <p> <table border=0 width=70%> <tr><td><b>PI:</b></td> <td>Peter C. Smith</td></tr> <tr><td> </td> <td>Coastal Ocean Science</td></tr> <tr><td> </td> <td>Bedford Institute of Oceanography</td></tr> <tr><td><b>Dataset:</b></td> <td>Eastern Gulf of Maine/Scotian Shelf</td></tr> <tr><td><b>Ships:</b></td> <td>CCS Parizeau, CCGS Hudson and CCGS Cygnus</td></tr> </table></p> <p> Note: Where available, see on-line cruise reports for additional information on<br> sampling and data processing. </p> <p><i> updated: April 8, 2004. G.Heimerdinger </i></p> CTD Data from Eastern Gulf of Maine/Scotian Shelf. 10128 mcm_ps mcm_ps http://globec.whoi.edu/jg/serv/globec/gb/mooring/mcm_ps.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/mcm_ps%7D <h2 align=center>Moored Current Meter Observations</h2> <p>In general, mooring locations and depths of current meters are redeployments of previous moorings. Thus, for some sites, the data record can be near continuous from 1993.</p> <p><b>Contributor:</b></br> Peter C. Smith<br> Bedford Institute of Oceanography<br> Dartmouth, Nova Scotia<br> CANADA</p> Moored Current Meter data from Peter Smith&#039;s cruises from Bedford Institute of Oceanography (BIO) 10129 moorings_GSC moorings_GSC http://globec.whoi.edu/jg/serv/globec/gb/mooring/moorings_GSC.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/moorings_GSC%7D <h4 align=center>Great South Channel Moorings, January to August, 1997</h4> <p><b>Contact information: </b>Ron Schlitz <br> NOAA/NMFS/NEFSC <br> 166 Water Street <br> Woods Hole, MA 02543 <br> 508-495-2395 <br> <a href="mailto:rschlitz@whsun1.wh.whoi.edu">rschlitz@whsun1.wh.whoi.edu</a> <br> FAX: 508-495-2258 </p> <hr> <p align=center><b>Notes:</b><br> Each mooring number below has information relevant to the data. </p> <pre> global attributes: :DATA_ORIGIN = "USGS" ; :MOORING = "4941" ; :DESCRIPT = "VACM-C, GREAT SOUTH CHANNEL SITE 1, CLEAN DATA: NOT SCRUBBED" ; :start_time = "97- I -16 13.33.45" ; :stop_time = "97- III-11 17.11.15" ; :latitude = 40.81667f ; :longitude = -68.15f ; THIS LONGITUDE IS INCORRECT. THE CORRECT LONGITUDE IS -69.15. :magnetic_variation = -17.f ; :sampling_interval = 450 ; :water_depth = 70.f ; :WATER_DEPTH = 70 ; :CREATION_DATE = "10:57 NOV 26,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4831" ; :DESCRIPT = "VACM GLOBEC GREAT SOUTH CHANNEL SITE 2" ; :start_time = "97- I -13 19.33.45" ; :stop_time = "97- VI -20 13.48.45" ; :latitude = 40.85417f ; :longitude = -68.81683f ; :magnetic_variation = -16.f ; :sampling_interval = 450 ; :water_depth = 72.f ; :WATER_DEPTH = 72 ; :CREATION_DATE = "10:07 DEC 2,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4832" ; :DESCRIPT = "VACM-C, GREAT SOUTH CHANNEL SITE 2, COMPASS TROUBLE STARTED " ; :start_time = "97- I -13 19.33.45" ; :stop_time = "97- III-27 07.11.15" ; :latitude = 40.85417f ; :longitude = -68.81683f ; :magnetic_variation = -16.f ; :sampling_interval = 450 ; :water_depth = 72.f ; :WATER_DEPTH = 72 ; :CREATION_DATE = "16:54 DEC 1,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4821" ; :DESCRIPT = "SEACAT, GREAT SOUTH CHANNEL SITE 3. CLEAN DATA, NOT SCRUBBE" ; :start_time = "97- I -13 16.35.00" ; :stop_time = "97- VI -20 17.25.00" ; :latitude = 40.8625f ; :longitude = -68.66683f ; :magnetic_variation = 0.f ; :sampling_interval = 600 ; :water_depth = 62.f ; :WATER_DEPTH = 62 ; :CREATION_DATE = "10:40 NOV 25,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4871" ; :DESCRIPT = "VMCM SITE 4 GREAT SOUTH CHANNEL. MANY WILD POINTS SCRUBBED. " ; :start_time = "97- I -14 20.31.52" ; :stop_time = "97- II -09 08.28.07" ; :latitude = 40.867f ; :longitude = -68.51017f ; :magnetic_variation = -16.56f ; :sampling_interval = 225 ; :water_depth = 52.f ; :WATER_DEPTH = 52 ; :CREATION_DATE = "15:10 MAR 7,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4921" ; :DESCRIPT = "SEACAT, GREAT SOUTH CHANNEL SITE 5. CLEAN DATA, NOT SCRUBBE" ; :start_time = "97- I -15 23.35.00" ; :stop_time = "97-VIII-20 17.25.00" ; :latitude = 40.71583f ; :longitude = -68.40667f ; :magnetic_variation = 0.f ; :sampling_interval = 600 ; :water_depth = 61.f ; :WATER_DEPTH = 61 ; :CREATION_DATE = "10:57 NOV 25,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4931" ; :DESCRIPT = "VACM-C, GREAT SOUTH CHANNEL SITE 6, CLEAN DATA: NOT SCRUBBED" ; :start_time = "97- I -16 03.33.45" ; :stop_time = "97-VIII-17 18.18.45" ; :latitude = 40.62683f ; :longitude = -68.356f ; :magnetic_variation = -17.f ; :sampling_interval = 450 ; :water_depth = 80.f ; :WATER_DEPTH = 80 ; :CREATION_DATE = "13:08 NOV 26,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4933" ; :DESCRIPT = "AANDERAA GREAT SOUTH CHANNEL SITE 6" ; :start_time = "97- I -16 04.41.00" ; :stop_time = "97- V -17 00.01.00" ; :latitude = 40.62683f ; :longitude = -68.356f ; :magnetic_variation = -17.f ; :sampling_interval = 1200 ; :water_depth = 80.f ; :WATER_DEPTH = 80 ; :CREATION_DATE = "13:26 DEC 10,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4901" ; :DESCRIPT = "VACM-C, GREAT SOUTH CHANNEL SITE 7, CLEAN DATA: NOT SCRUBBED" ; :start_time = "97- I -15 19.33.45" ; :stop_time = "97-VIII-17 09.56.15" ; :latitude = 40.51683f ; :longitude = -68.28616f ; :magnetic_variation = -17.f ; :sampling_interval = 450 ; :water_depth = 101.f ; :WATER_DEPTH = 101 ; :CREATION_DATE = "09:13 DEC 1,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4902" ; :DESCRIPT = "VACM GLOBEC GREAT SOUTH CHANNEL SITE 7" ; :start_time = "97- I -15 19.33.45" ; :stop_time = "97-VIII-17 09.26.15" ; :latitude = 40.51683f ; :longitude = -68.28616f ; :magnetic_variation = -17.f ; :sampling_interval = 450 ; :water_depth = 101.f ; :WATER_DEPTH = 101 ; :CREATION_DATE = "13:33 DEC 5,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4903" ; :DESCRIPT = "AANDERAA GREAT SOUTH CHANNEL SITE 7. CLEAN DATA, NOT SCRUBB" ; :start_time = "97- I -15 23.41.00" ; :stop_time = "97- V -14 00.21.00" ; :latitude = 40.51683f ; :longitude = -68.28616f ; :magnetic_variation = -16.f ; :sampling_interval = 1200 ; :water_depth = 101.f ; :WATER_DEPTH = 101 ; :CREATION_DATE = "13:53 DEC 10,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4892" ; :DESCRIPT = "MX-VACM, GREAT SOUTH CHANNEL SITE 8. NO ROTOR, MOORING FELL" ; :start_time = "97- I -15 16.33.45" ; :stop_time = "97- II -11 22.26.15" ; :latitude = 40.24533f ; :longitude = -68.17f ; :magnetic_variation = -16.5f ; :sampling_interval = 450 ; :water_depth = 325.f ; :WATER_DEPTH = 325 ; :CREATION_DATE = "16:31 FEB 6,\'98" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4893" ; :DESCRIPT = "AANDERAA GREAT SOUTH CHANNEL SITE 8. MOORING FELL 2/12. " ; :start_time = "97- I -15 15.42.00" ; :stop_time = "97- II -12 01.42.00" ; :latitude = 40.24533f ; :longitude = -68.17f ; :magnetic_variation = -16.f ; :sampling_interval = 1200 ; :water_depth = 325.f ; :WATER_DEPTH = 325 ; :CREATION_DATE = "13:51 DEC 10,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4894" ; :DESCRIPT = "AANDERAA GREAT SOUTH CHANNEL SITE 8. MOORING FELL 2/12." ; :start_time = "97- I -15 16.40.00" ; :stop_time = "97- II -12 01.40.00" ; :latitude = 40.24533f ; :longitude = -68.17f ; :magnetic_variation = -16.f ; :sampling_interval = 1200 ; :water_depth = 325.f ; :WATER_DEPTH = 325 ; :CREATION_DATE = "13:47 DEC 10,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; :DATA_ORIGIN = "USGS" ; :MOORING = "4841" ; :DESCRIPT = "VACM GLOBEC GREAT SOUTH CHANNEL SITE 9" ; :start_time = "97- I -14 00.33.45" ; :stop_time = "97- VI -21 22.48.45" ; :latitude = 40.70033f ; :longitude = -68.67533f ; :magnetic_variation = -16.f ; :sampling_interval = 450 ; :water_depth = 61.f ; :WATER_DEPTH = 61 ; :CREATION_DATE = "11:06 DEC 2,\'97" ; :DATA_TYPE = "TIME" ; :COORD_SYSTEM = "GEOGRAPHICAL" ; </pre> 10130 mooring_ef mooring_ef http://globec.whoi.edu/jg/serv/globec/gb/mooring/mooring_ef.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/mooring_ef%7D <h2 align=center>Georges Bank Eastern Flank Mooring Arrays<br> 1998-1999</h2> <p> Array Summary: <br> The Georges Bank moored instrument array (East Flank) was moored at ~41.7N and 66.1W in ~90m of water. The array consisted of a Toroid mooring (EFT) Nov 98 - Mar 99, an instrumented Guard mooring (EFG) Mar 99 - Aug 99, and a replacement Discus mooring (EFD) for the Toroid Mar 99 - August 99. The Toroid and Discus moorings were instrumented with temperature sensors at 10, 20, 45 meters; CTD units at 1, 15, 80 meters; and current meter units at 5 and 25 meters. The Guard mooring was instrumented with a temperature sensor at 1 meter. <p> <b>DMO Notes:</b><br> 1.. On mooring EFT (East Flank Toroid) yearday values are numbered consecutively from Nov 1998 to Mar 1999.<br> 2.. At the present time, the values for u and v are not available.<br> 3..These data are served from the orginal Matlab binary files. But for performance reasons, a cached version of these data (in JGOFS/GLOBEC format) is used. Missing data are represented as either "nd" or as "NaN". <br> <br> <b>Questions regarding these data should be directed to:</b><br> Richard Limeburner<br> Woods Hole Oceanographic Institution<br> Woods Hole, MA 02543<br><br> Phone: 508 289 2539 <br> E-mail: <a href="mailto:rlimeburner@whoi.edu">rlimeburner@whoi.edu</a><br> <p> <pre> <b>PI Notes:</b> The original processing comments from the file readme.txt are show below: For edited raw data at EF mooring R. Limeburner 7/30/01 Input - Galbraith's *s.mat converted ascii raw data, time corrected Output - *se.mat, with start/stop time in phase, big spikes interpolated See plots eftraw.jpg, efsraw.jpg, eftlp.jpg, efslp.jpg NEP Edited Raw Data 2001 Filename Start time Stop Time Comment EFTbt10m1800se.mat 111798 140000 031199 190000 ok EFTbt20m1800se.mat 111798 140000 031199 190000 ok EFTbt45m1800se.mat 111798 140000 031199 190000 ok EFTsc1m300se.mat 111798 140000 031199 190000 ok, may need Flagg editing EFTsc15m450se.mat 111798 140000 031199 190000 ok, may need Flagg editing EFTsc80m450se.mat 111798 140000 031199 190000 ok, may need Flagg editing EFTvm5m450se.mat 111798 140000 031199 190000 ok EFTvm25m450se.mat 111798 140000 031199 190000 ok EFDbt10m900se.mat 033099 020000 080399 160000 ok EFDbt20m900se.mat 033099 020000 080399 160000 ok EFDbt45m900se.mat 033099 020000 080399 160000 ok EFDbt60m900se.mat 033099 020000 042799 044500 may need more editing EFDsc2m120se.mat 033099 020000 073199 065600 ok, may need Flagg editing EFDsc15m225se.mat 033099 020000 062799 110000 ok, may need Flagg editing EFDsc35m225se.mat 033099 020000 071099 183000 ok, may need Flagg editing EFDsc80m225se.mat 033099 020000 080399 160000 ok, may need Flagg editing EFDvm5m450se.mat 033099 020000 080399 160000 temp much shorter than velocity EFDvm25m450se.mat 033099 020000 051999 223730 ok Editing EF history 1. Input GAlbraiths 7/26/01 data set with correct time 2. ETTsc1m330s.mat, fix cond spike at cond(12638), cond(18798) delete data(32895:32919), delete data(1) corrects the start time. 3 EFTsc15m450s.mat ok 4. EFTsc80m450s.mat data(21930:21945)=[] fixes time b=wild(temp,200,5.0); b=wild(sal,200,5.0); b=wild(sigma,200,5.0);10m 5. EFTbt 5. EFTvm25m450s.mat b=wild(north,200,3.0); temp(15033:21929)=[]; 7. EFDsc2m120s.mat data(88710:91141)=[]; 8. EFDsc15m225s.mat temp(34322:48609)=[]; b=wild(sal,200,5.0); ;b=wild(sigma,200,5.0); 8. EFTsc35m225s.mat b=wild(temp,200,5); b=wild(temp,100,9); b=wild(sal,200,5); b=wild(sal,200,7); b=wild(sigma,200,7); b=wild(sigma,200,7); </pre> <p> <i>Last updated April 6, 2006</i> </pre> 10131 NEP1995 NEP1995 http://globec.whoi.edu/jg/serv/globec/gb/mooring/NEP1995.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/NEP1995%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>N.E. Peak Mooring Site <br> 41 44' N, 66 32' W</h3> <p> The data reported here are for those data obtained by the N.E.Peak mooring deployment of Nov 1 1995 to Mar 30 1996. <p> <pre> <b>Note:</b> Sampling rates vary from instrument to instrument and depth to depth. <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> 1. The nominal position of the mooring is the designed deployment site and actual deployments varied by about 0.5 nm around this position. 2. Sensor depths are nominal designed depths. In water sensors vary around this designed depth by about 1 m, variation larger at greater distance below buoy. 3. Temperatures are listed in the IPTS68 standard, rather than IPT90. 4. Salinity conversion from conductivity was done with PSS78 5. Sensor normalization was done with pre-cruise calibrations, and checked with post-cruise calibrations. 6. Only minor editing has been done to remove spikes from records. 7. No corrections have been made to fluorometer and transmissometer data to remove biological fouling induced drift. 8. No corrections have been made to salinity for drifts due to biological fouling. <i> updated 08/10/05; gfh</i></pre> 10132 NEP1996 NEP1996 http://globec.whoi.edu/jg/serv/globec/gb/mooring/NEP1996.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/NEP1996%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>N.E. Peak Mooring Site <br> 41 44' N, 66 32' W</h3> <p> Two deployments were made in 1996 at this site. The first deployment was between Apr 07, 1996 and Apr 17, 1996. The second deployment was between Oct 29, 1996 and Dec 19, 1996. (Dates reflect dates of data not deployment time) <p> <pre> <b>Notes:</b> ¹Light transmission at 10 meters from the first deployment 1n 1996<br> is reported as volts. Sampling rates vary from instrument to instrument and depth to depth. <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> 1. The nominal position of the mooring is the designed deployment site and actual deployments varied by about 0.5 nm around this position. 2. Sensor depths are nominal designed depths. In water sensors vary around this designed depth by about 1 m, variation larger at greater distance below buoy. 3. Temperatures are listed in the IPTS68 standard, rather than IPT90. 4. Salinity conversion from conductivity was done with PSS78 5. Sensor normalization was done with pre-cruise calibrations, and checked with post-cruise calibrations. 6. Only minor editing has been done to remove spikes from records. 7. No corrections have been made to fluorometer and transmissometer data to remove biological fouling induced drift. 8. No corrections have been made to salinity for drifts due to biological fouling. <i> updated 06/15/05; gfh</i></pre> 10133 NEP1997 NEP1997 http://globec.whoi.edu/jg/serv/globec/gb/mooring/NEP1997.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/NEP1997%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>N.E. Peak Mooring Site <br> 41 44' N, 66 32' W</h3> <p> One deployment was made in 1997 at this site, Feb 18 to Jun 29 1997. (dates reflect dates of data not deployment time) <p> <pre> <b>Note:</b> Sampling rates vary from instrument to instrument. <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> 1. The nominal position of the mooring is the designed deployment site and actual deployments varied by about 0.5 nm around this position. 2. Sensor depths are nominal designed depths. In water sensors vary around this designed depth by about 1 m, variation larger at greater distance below buoy. 3. Temperatures are listed in the IPTS68 standard, rather than IPT90. 4. Salinity conversion from conductivity was done with PSS78 5. Sensor normalization was done with pre-cruise calibrations, and checked with post-cruise calibrations. 6. Only minor editing has been done to remove spikes from records. 7. No corrections have been made to fluorometer and transmissometer data to remove biological fouling induced drift. 8. No corrections have been made to salinity for drifts due to biological fouling. <i> updated 06/15/05; g.heimerdinger</i></pre> 10134 NEP1998 NEP1998 http://globec.whoi.edu/jg/serv/globec/gb/mooring/NEP1998.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/NEP1998%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>N.E. Peak Mooring Site <br> 41 44' N, 66 32' W</h3> <p> One deployment was made in 1998 at this site, Nov 19. 1998 to Mar 11 1999. (Dates reflect dates of data not deployment dates) <p> <pre> <b>Note:</b> Sampling rates vary from instrument to instrument. <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> 1. The nominal position of the mooring is the designed deployment site and actual deployments varied by about 0.5 nm around this position. 2. Sensor depths are nominal designed depths. In water sensors vary around this designed depth by about 1 m, variation larger at greater distance below buoy. 3. Temperatures are listed in the IPTS68 standard, rather than IPT90. 4. Salinity conversion from conductivity was done with PSS78 5. Sensor normalization was done with pre-cruise calibrations, and checked with post-cruise calibrations. 6. Only minor editing has been done to remove spikes from records. 7. No corrections have been made to fluorometer and transmissometer data to remove biological fouling induced drift. 8. No corrections have been made to salinity for drifts due to biological fouling. <i> updated 06/15/05; gfh</i></pre> 10135 NEP1999 NEP1999 http://globec.whoi.edu/jg/serv/globec/gb/mooring/NEP1999.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/NEP1999%7D <h3 align=center>GLOBEC Georges Bank Long-term Moored Array Component</h3> <h3 align=center>N.E. Peak Mooring Site <br> 41 44' N, 66 32' W</h3> <p> One deployment was made in 1999 at this site, Mar 12. 1999 to Aug 14 1999. (Dates reflect dates of data not deployment time) <p> <pre> <b>Note:</b> Sampling rates vary from instrument to instrument. <b>Data Submitted by:</b> Jim Irish Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: 508 289 2732 fax: 508 457 2195 e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a> 1. The nominal position of the mooring is the designed deployment site and actual deployments varied by about 0.5 nm around this position. 2. Sensor depths are nominal designed depths. In water sensors vary around this designed depth by about 1 m, variation larger at greater distance below buoy. 3. Temperatures are listed in the IPTS68 standard, rather than IPT90. 4. Salinity conversion from conductivity was done with PSS78 5. Sensor normalization was done with pre-cruise calibrations, and checked with post-cruise calibrations. 6. Only minor editing has been done to remove spikes from records. 7. No corrections have been made to fluorometer and transmissometer data to remove biological fouling induced drift. 8. No corrections have been made to salinity for drifts due to biological fouling. <i> updated 08/10/05; gfh</i></pre> 10136 SF_vel_temp SF_vel_temp http://globec.whoi.edu/jg/serv/globec/gb/mooring/1999/SF_vel_temp.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/SF_vel_temp%7D These movies depict low pass filtered velocity and temperature data from the southern flank of Georges Bank in 1999. The movies have been broken up between the spring (3/21/1999-6/10/1999) and summer (6/18/1999-8/30/1999) deployments. The instruments were moved slightly south east for the summer deployment (see <a href="http://usjgofs.whoi.edu/movies/schlitz/mooring_positions.html">Mooring Positions</a>). The instruments were deployed colinearly roughly orthogonal to the isobaths. Velocity was measured with seven broadband (300 KHz) workhorse ADCPs which were mounted on tripods on the ocean bottom. Temperature was measured with strings of vemco temperature probes, brankers, and the internal temperature sensors on the ADCPs. The vertical and horizontal position of the instruments recovered after each deployment are depicted in <a href="http://usjgofs.whoi.edu/movies/schlitz/spring_array.jpg">spring_array.jpg</a> and <a href="http://usjgofs.whoi.edu/movies/schlitz/summer_array.jpg">summer_array.jpg</a> (see <a href="http://usjgofs.whoi.edu/movies/schlitz/spring_array.gif">spring_array.gif</a> and <a href="http://usjgofs.whoi.edu/movies/schlitz/summer_array.gif">summer_array.gif</a> for gif versions.) The time between frames in each movie is one hour. All contouring and quiver plots used bilinear interpolation. <p> <b>spring/summer_velocity.fli:</b> The top of each frame in this movie depicts the low passed three dimensional velocity field. The along bank (75 degrees clockwise from north) velocity is contoured with a contour interval of one cm/sec, a colorbar on the right gives the scale. Positive velocities (red) are up bank, to the east-north east. The cross bank (165 degrees clockwise from north) and vertical velocity are depicted by a two dimensional vector field with a scale given in the lower left hand corner. The topography shown in this frame is a about four meters higher than in reality to cover the edge artifacts in the countouring. At the bottom of the frame is a stick plot of the previous 48 hours of wind. The wind vectors are oriented so that up is north and to the right of the screen is to the east. the vectors move backwards in time from the right of the screen to the left. <p> <b>spring/summer_velocity_temperature.fli:</b> The top and bottom window of each movie frame are the same as those decribed in spring_1999_SFGB_velocity.fli. The middle window contains a contour of the low passed temperature data. The temperature is contoured with half a degree Celsius contour intervals, the temperature scale is given by the colorbar to the right. <p> A few artifacts in these films * Because of surface elevation changes the top bin of the ADCP's often give false measurements. Please interperet velocity measurements in the top 5 meters of the water column with a grain of salt. <p> **The branker temperature probe at one meter depth site 2 failed towards the end of the first deployment causing the odd temperature contour at the end of the movie spring_1999_SFGB_velocity_temperature.fli. <p> *** All movies are in FLI format which can be viewed with xanim on a unix platform or with PowerFliC on a PC. A zipped copy of PowerFLiC is available in the file <a href="http://usjgofs.whoi.edu/movies/schlitz/pwflc252.zip"> pwflc252.zip</a>. <p> For further information contact: Keston Smith (<a href="mailto:ksmith@whsun1.wh.whoi.edu">ksmith@whsun1.wh.whoi.edu</a>) or Ron Schlitz (<a href="mailto:rschlitz@whsun1.wh.whoi.edu">rschlitz@whsun1.wh.whoi.edu</a>) </pre> 10137 sss sss http://globec.whoi.edu/jg/serv/globec/gb/mooring/1994/sss.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/sss%7D <pre> <p><b>PI:</b> J. Irish </p> <p><b>Dataset:</b> Sea surface sensor data </p> <p><b>Ship:</b> Endeavor </p> <p><b>Cruise:</b> 256 </p> <br> <p><b>Data submitted by:</b></p> <p>Jim Irish</p> <p>Woods Hole Oceanographic Institution</p> <p>Woods Hole, MA 02543</p> <br> <p>phone: 508 289 2732</p> <p>fax: 508 457 2195</p> <p>e-mail: <a href="mailto:jirish@whoi.edu">jirish@whoi.edu</a></p> </pre> <br> Last updated 7,January,2009 Jim Irish sea surface temperature, salinity and fluorometer data <pre> # * Sea-Bird SBE 21 Data File: # * FileName = C:TSALDATAEN256B.HEX # * Software Version 4.205 # * Temperature SN = 1578 # * Conductivity SN = 1578 # * System UpLoad Time = Oct 30 1994 00:37:51 # * R/V Endeavor # * Thermosalinograph # nquan = 5 # nvalues = 2134 # units = metric # name 0 = timeJ: time [julian days] # name 1 = t068: temperature, IPTS-68 [deg C] # name 2 = sal: salinity, PSS-78 [PSU] # name 3 = v0: voltage, number 0 [V] # name 4 = flag: 0.000e+00 # span 0 = 303.02628, 304.50754 # span 1 = 12.0186, 20.5458 # span 2 = 31.3208, 35.1059 # span 3 = 0.460, 1.521 # span 4 = 0.000e+00, 0.000e+00 # interval = seconds: 60 # start_time = Oct 30 1994 00:37:51 # bad_flag = -9.990e-29 # serial_numbers = t0:1578, c0:1578, upoly1:TFluor # datcnv_date = Oct 31 1994 12:04:12, 4.205 # datcnv_in = EN256B.HEX EN256B.CON 1578 1578 # datcnv_skipover = 0 # file_type = ascii # *END* </pre> 10138 st2mooring st2mooring http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/mooring.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/mooring/,info=globec.whoi.edu/jg/info/globec/gb/mooring/st2mooring%7D <h2 align=center> Acoustic Doppler Current Profiler Observations </H2> <h2 align=center>Current Vectors, April - June 1995</H2> <pre> <b>Ship:</B> R/V Seward Johnson <b>Cruises/Dates:</b> SJ9506/April 26 - May 2, 1995 SJ9508/June 6 - 16, 1995 <b>Instruments:</b> RDI, broadband 150 and 600 kHz ADCP units RDI, narrowband 150 kHz ADCP unit <b>obs. modes:</b> on-station and along track See file comments for specifics on instruments used, observational modes and data averaging intervals. </Pre> <p><pre> Prepared by: Russ Burgett, URI <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 voice: 401 874 6610 fax: 401 874 6728 email: <a href="mailto:hebert@gso.uri.edu">hebert@gso.uri.edu</a> <i>Updated: August 27, 2004; gfh</i> </pre> 10139 allADCP allADCP http://globec.whoi.edu/jg/serv/globec/gb/process/1995/allADCP.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/allADCP%7D <h2 align=center> Acoustic Doppler Current Profiler Observations </H2> <h2 align=center>Current Vectors, April - June 1995</H2> <pre> <b>Ship:</B> R/V Seward Johnson <b>Cruises/Dates:</b> SJ9506/April 26 - May 2, 1995 SJ9508/June 6 - 16, 1995 <b>Instruments:</b> RDI, broadband 150 and 600 kHz ADCP units RDI, narrowband 150 kHz ADCP unit <b>obs. modes:</b> on-station and along track See file comments for specifics on instruments used, observational modes and data averaging intervals. </Pre> <p><pre> Prepared by: Russ Burgett, URI <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 voice: 401 874 6610 fax: 401 874 6728 email: <a href="mailto:hebert@gso.uri.edu">hebert@gso.uri.edu</a> <i>Updated: August 27, 2004; gfh</i> </pre> SJ9508 NB 150 kHz ADCP 5 minute average 10140 alongtrackel alongtrackel http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/el_shipdata.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/alongtrackel%7D <h2 align=center> Edwin Link Cruises: 9904 and 9905<br> Shipboard meteorology and sea surface measurements<br> along the ship's track<br></h2> <pre> <b>Data submitted by:</b> James Manning National Marine Fisheries Service, NEFC Woods Hole, MA 02543 voice: 508-495-2211 fax: 508-495-2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> </pre> <p> Note: Karen Fisher (Cornell Univ.) played the major role in processing our EDWIN LINK alongtrack data. I have simply modified and executed her Perl routines to comply with GLOBEC standards. <b>Very little cleaning of the raw data was conducted (Jan 2000 Jim Manning). </b> <p> <i>Last modified: Sept 30, 2005; gfh w/ input from J.Manning</i> </pre> GLOBEC Georges Bank Cruises EDWIN LINK Shipboard Sensor Data ~ 1 minute intervals. 10141 alongtrackoc alongtrackoc http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/oc_shipdata.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/alongtrackoc%7D <h2 align=center> Oceanus Cruises: 296, 301 and 303<br> Shipboard meteorology and sea surface measurements<br> along the ship's track<br></h2> <p> <b>Note:</b><br>I (Jim Manning) suggest that investigators use Dick Payne's version of OCEANUS alongtrack data. The raw data I post here was processed primarily while underway and has obvious problems. There are unrealistic (sometimes negative) temperature and eratic salinity. Winds are of especially poor quality as noted below.</b><br><br> I have been delayed in getting this data on-line because I am not happy with my "corrected" wind (with ships motion removed) and, I am still not comfortable with posting the corrected wind so I have added a comment on the fact that it is questionable. I have notified the OCEANUS SSSG people about this problem. In the meantime I suggest that any one interested in wind for these periods use the NOAA buoy winds or Dick Paynes OCEANUS alongtrack data instead. </p> <pre> <b>Data submitted by:</b> James Manning National Marine Fisheries Service NOAA Woods Hole, MA 02543 voice: 508-495-2211 fax: 508-495-2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> <i>Last modified: Sept 16, 2005; gfh w/ input from J.Manning</i></pre> GLOBEC Georges Bank Cruises OCEANUS Shipboard Sensor Data. Cleaned and merged to 1 minute intervals 10142 alongtracksj alongtracksj http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/sj_shipdata.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/alongtracksj%7D <h2 align=center> Seward Johnson Cruises: 9505 and 9507<br> Shipboard meteorology and sea surface measurements<br> along the ship's track<br></h2> <pre> <b>Note: As noted below, these data are uncalibrated and should be used accordingly.</b> <b>Data submitted by:</b> Jim Manning National Marine Fisheries Service NOAA Woods Hole, MA 02543 </pre> <p> <ol> <li> These data are accessed under the the GLOBEC homepage-->data-->process-->{year}-->alongtrack <li> These are stored as single ascii files per cruise with several variables merged to one minute (interpolated) time steps. <li> The first column is the time stamp which, for Albatross convention, is "yrday0_gmt" which means, for example, that a time of "0.5" represents local noontime on Jan 1st. <li> We all understand this data (shipboard temp, salt, wind, etc.) should be treated as uncalibrated records and <b>should not be used other than exploratory purposes</b>. </ol> <p> <i>updated 09/15/05; gfh w/ input by J.Manning</i> </pre> GLOBEC Georges Bank Cruises Shipboard Sensor Data. Cleaned and merged to 5 minute intervals. 10143 chlor_phaeo chlor_phaeo http://globec.whoi.edu/jg/serv/globec/gb/process/1995/chlor_phaeo.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/chlor_phaeo%7D <h2 align=center>Extracted Chlorophyll and Phaeopigment</h2> <p> <b>DMO note:</b> The data reported consists of three replicates per each depth horizon sampled. </p> <P><b>PI Responsible: Dian J. Gifford</b> <P>Samples for water column chlorophyll and phaeopigment were collected and analyzed during the following Vital rates 1995 U.S. GLOBEC Georges Bank process cruises:</P> <li>EN259 <li>EN262 <li>EN264 <li>EN266 <li>EN267B (aka EN267II and EN267 LEG 2) </ul> <P>Water Collection: Seawater was collected using 10-L teflon-lined Go-flo bottles mounted on the Neil Brown CTD rosette. Water was drained into opaque brown 1-L bottles immediately after collection and refrigerated until processed. Samples were collected onto filters within one hour of water collection. In areas where the water column was well mixed, water was collected from the top, middle and bottom of the water column. When the water column was stratified, water was collected from the top, middles and bottom of the water column as well as around the hydrographic features of interest.</P> <P>Sample Processing: Samples were prepared for total, &lt;20 &micro;m, and &lt;5 &micro;m chlorophyll and phaeopigment. Samples for total pigments consisted of bulk seawater. Samples for &lt; 20 &micro;m and &lt; 5 &micro;m pigments were passed gently through clean Nitex meshes of appropriate porosity and the filtrate retained for analysis. Three replicate 50-ml samples of each size fraction were collected onto 25 mm GF/F filters, placed into 5 ml of 90% acetone in a capped test tube, and extracted in the freezer for 24 hours prior to analysis.</P> <P>Sample Analysis: The filters were removed from defrosted test tubes with a clean stainless steel spatula, the tube wiped clean with a Kimwipe, and samples read on a Turner Designs Model 10 fluorometer before and after acidification with 10% HCl (Parsons et al., 1984).</P> <P>Caveat: In general, pigment concentrations in the &lt;5 &micro;m samples were approximately equal to the &lt;20 &micro;m samples (i.e., there was very little chlorophyll in the 5-20 &micro;m size range: most chlorophyll &lt; 20 &micro;m was also &lt; 5 &micro;m). Because of the difficulty of passing seawater quantitatively through the 5 &micro;m mesh, the &lt;5 &micro;m data are more variable than the Total and &lt; 20 &micro;m data. To avoid confusion, the &lt; 5 &micro;m data are not included in the data files. The data are available, and scientific investigators who need it should contact the PI directly.</P> <P>Data Use: The data are available for use by any scientific investigator who wishes to use them. The PI must be consulted prior to publication.</P> <pre> <b>Data Submitted by:</b> Dian J. Gifford Graduate School of Oceanography University of Rhode Island Narragansett, RI 02882-1197 voice: 401-874-6690 fax: 401-874-6240 e-mail: <a href="mailto:gifford@gsosun1.gso.uri.edu">gifford@gsosun1.gso.uri.edu</a> <i> updated: Aug 05. 2005, gfh</i> </pre> Seawater was collected using 10-L teflon-lined Go-flo bottles mounted on the Neil Brown CTD rosette. Water was drained into opaque brown 1-L bottles immediately after collection and refrigerated until processed. Samples were collected onto filters within one hour of water collection. In areas where the water column was well mixed, water was collected from the top, middle and bottom of the water column. When the water column was stratified, water was collected from the top, middles and bottom of the water column as well as around the hydrographic features of interest. <p>Sample Processing: Samples were prepared for total, &lt;20 µm, and &lt;5 µm chlorophyll and phaeopigment. Samples for total pigments consisted of bulk seawater. Samples for &lt; 20 µm and &lt; 5 µm pigments were passed gently through clean Nitex meshes of appropriate porosity and the filtrate retained for analysis. Three replicate 50-ml samples of each size fraction were collected onto 25 mm GF/F filters, placed into 5 ml of 90% acetone in a capped test tube, and extracted in the freezer for 24 hours prior to analysis.</p> <p>Sample Analysis: The filters were removed from defrosted test tubes with a clean stainless steel spatula, the tube wiped clean with a Kimwipe, and samples read on a Turner Designs Model 10 fluorometer before and after acidification with 10% HCl (Parsons et al., 1984).</p> <p>Caveat: In general, pigment concentrations in the &lt;5 µm samples were approximately equal to the &lt;20 µm samples (i.e., there was very little chlorophyll in the 5-20 µm size range: most chlorophyll &lt; 20 µm was also &lt; 5 µm). Because of the difficulty of passing seawater quantitatively through the 5 µm mesh, the &lt;5 µm data are more variable than the Total and &lt; 20 µm data. To avoid confusion, the &lt; 5 µm data are not included in the data files. The data are available, and scientific investigators who need it should contact the PI directly.</p> 10144 chlorophyll chlorophyll http://globec.whoi.edu/jg/serv/globec/gb/process/chlorophyll.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/chlorophyll%7D <h3 align=center> Chlorophyll data from R/V Endeavor 321 and 325</h3> </p> The pigments were analyzed by fluorometry according to <b>Parsons et al.</b> 1984, "<u>A Manual of Chemical and Biological Methods for Seawater Analysis.</u>" Pergamon Press, New York. </p> <pre> <b>Data submitted by:</b> Dr. Dian J. Gifford Graduate School of Oceanography University of Rhode Island Narragansett, RI 02882-1197 phone: 401-874-6690 fax: 401-874-6240 e-mail: <a href="mailto:gifford@gsosun1.gso.uri.edu">gifford@gsosun1.gso.uri.edu</a> <i> updated: gfh, July 14, 2004 </i></pre> Chlorophyll data from Dian Gifford&#039;s Georges Bank Cruise R/V Endeavor EN325. The pigments were analyzed by fluorometry according to Parsons et al. 1984, "A Manual of Chemical and Biological Methods for Seawater Analysis." Pergamon Press, New York. 10145 ctd_dh ctd_dh http://globec.whoi.edu/jg/serv/globec/gb/process/1995/ctd_dh.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/ctd_dh%7D <h2 align=center>CTD Observations, 1995 Seward Johnson Process Cruises</h2> <p> <b>CTD Processing Notes and Comments:</b> <p> <hr> <p><b> Re: SJ9506 </b> <p>Seward Johnson cruise <b>SJ9506</b> 25 Apr - 3 May 1995; using the (NBIS Mark III) CTD system. <p>Calibrated CTD files provided by R. Limeburner, WHOI. <p> <hr> <p><b> Re: SJ9508 </b> <p> Seward Johnson cruise <b>SJ9508</b> 6 - 16 June 1995; using the (NBIS Mark III) CTD system. <p>Calibrated CTD files were prepared by R. Limeburner except for stations 1, 37, 51 and 61 which were processed by Russ Burgett, URI.</p> <p>There was no station 95 for this cruise. <p>Examination of the files showed the salinity (and sigma_t) to be suspect. The salinty and sigma_t fields have been manually edited and obvious problems marked as no data (nd), however care should be taken when using the salinity and sigma_t from these files. Pressure, temperature, salinity and sigma_t from a SeaBird CTD added to the Seward Johnson CTD package are available for casts 112-114, 116, 124-128, 130-136, 138-140, 142-151, 153-160, 162, 164-172, and 174-185. It is recommended to use these files when possible. They are available as a separate object.</p> <p>Examination of the unprocessed CTD files showed a 4 dbar pressure offset in the CTD calibration. This offset was added to the pressure in the calibrated files.</p> <p> <hr> <p><b> Re: SJ9508sb </b> <p> Seward Johnson cruise <b>SJ9508</b> 6 - 16 June 1995; using the (Seabird SBE-25) CTD system. <p>The Seabird CTD was added to the Seward Johnson CTD package after cast 111 due to poor quality conductivity data. Seabird casts 112-114, 116, 124-128, 130-136, 138-140, 142-151, 153-160, 162, 164-172, and 174-185 are available in this data set.</p> <hr> <pre> <b>Contributor:</b> David Hebert University of Rhode Island Graduate School of Oceanography Narragansett, RI 02882-1197 voice: 401 874 6610 fax: 401 874 6728 email: <a href="mailto:hebert@gso.uri.edu">hebert@gso.uri.edu</a> <b>Data Prepared by:</b> Russ Burgett University of Rhode Island Graduate School of Oceanography <i>Updated December 1, 2004; gfh</i> </pre> SJ9508 Seabird CTD Stations. Using the (Seabird SBE-25) CTD system. <p>Calibrated CTD files were prepared by R. Limeburner except for stations 1, 37, 51 and 61 which were processed by Russ Burgett, URI.</p> <p>There was no station 95 for this cruise. </p><p>Examination of the files showed the salinity (and sigma_t) to be suspect. The salinty and sigma_t fields have been manually edited and obvious problems marked as no data (nd), however care should be taken when using the salinity and sigma_t from these files. Pressure, temperature, salinity and sigma_t from a SeaBird CTD added to the Seward Johnson CTD package are available for casts 112-114, 116, 124-128, 130-136, 138-140, 142-151, 153-160, 162, 164-172, and 174-185. It is recommended to use these files when possible. They are available as a separate object.</p> <p>Examination of the unprocessed CTD files showed a 4 dbar pressure offset in the CTD calibration. This offset was added to the pressure in the calibrated files.</p> 10146 ctd_fv ctd_fv http://globec.whoi.edu/jg/serv/globec/gb/process/ctd_fv.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/ctd_fv%7D <h2 align=center>Fishing Vessel CTD Data, Gulf of Maine</h2> <p> Note: The Brunt-Vaisala Frequency (N-squared) data were reprocessed by Frank Bub with raw data calculated over 1 m intervals, rather than smoothed over 5 m bins. The 5 m bins did not work well with inshore profiles. Negative numbers indicate instability. Use data with caution. <p> <p> <table border=0> <tr><td><B>Contacts:</B></td> <td>James J. Pierson, Ann Bucklin and Frank Bub</td></tr> <tr><td> </td> <td>Univ. of New Hampshire</td></tr> <tr><td><B>Ship:</B></td> <td>F/V Susan & Caitlyn</td></tr> </table> <body> <p> <br> The UNH SeaBird SBE-25 SeaLogger measures: <p> <ul> <li>Temperature (degrees C) with a SeaBird SBE-3F. <li>Conductivity (Siemens/m) with a SeaBird SBE-4C. <li>Pressure (decibars) with a SBE 29 strain gage sensor. <li>Percent light transmission with a Wet Labs CST-126R transmissometer across a 25 cm distance at the red light wavelength 660 nm. Data are presented as a percentage relative to pure water. <li>Chlorophyll concentration in micrograms/liter with a Wet Labs WETStar Fluorometer model 9607003. <li>PAR (photosynthetically active radiation) with a Biospherical QPS-200PD which observes an upper hemispherical total irradiance in quanta/sq-cm/sec. <li>Dissolved oxygen with a SBE-23Y (Yellow Springs Instrument) in milliliters/liter. </ul> <p> During a cast, sensors are flushed with a SBE-5T pump at approximately 25 ml/s. The system samples and stores all data at 8 Hz (8 samples/ second). Profiling rates should be 20 meters/minute for an average of 24 samples/1 m pressure level. Normally only the downcasts are analyzed (unless a problem is noted). Sensors are factory calibrated annually. <p> Derived data are calculated using Matlab and/or UNH algorithms developed in accordance with standards prescribed by Fofonoff and Millard, 1983. <p> For additional information about the SC9801 cruise see the <a href="http://globec.whoi.edu/globec-dir/reports/sc9801/progress_report.html"> NOAA Coastal Ocean Program Progress Report</a> <p> Additional <a href="http://globec.whoi.edu/globec-dir/data_doc/fishing_vessel_ctd.txt">data processing notes</a> were provided by the contributor. Note: These notes reflect the CTD processing steps for data collected during the UNH CONVEX progam. However, they are indicative of the processing performed on the data reported here. Parameter names have been changed to agree with GLOBEC requirements. </body> <p> <br> <i>updated: October 12, 2004; G.Heimerdinger </i></p> </pre> The UNH SeaBird SBE-25 SeaLogger measures: <p><ul> <li>Temperature (degrees C) with a SeaBird SBE-3F. </li><li>Conductivity (Siemens/m) with a SeaBird SBE-4C. </li><li>Pressure (decibars) with a SBE 29 strain gage sensor. </li><li>Percent light transmission with a Wet Labs CST-126R transmissometer across a 25 cm distance at the red light wavelength 660 nm. Data are presented as a percentage relative to pure water. </li><li>Chlorophyll concentration in micrograms/liter with a Wet Labs WETStar Fluorometer model 9607003. </li><li>PAR (photosynthetically active radiation) with a Biospherical QPS-200PD which observes an upper hemispherical total irradiance in quanta/sq-cm/sec. </li><li>Dissolved oxygen with a SBE-23Y (Yellow Springs Instrument) in milliliters/liter. </li></ul> <p> During a cast, sensors are flushed with a SBE-5T pump at approximately 25 ml/s. The system samples and stores all data at 8 Hz (8 samples/ second). Profiling rates should be 20 meters/minute for an average of 24 samples/1 m pressure level. Normally only the downcasts are analyzed (unless a problem is noted). Sensors are factory calibrated annually. </p> <p> Note: The Brunt-Vaisala Frequency (N-squared) data were reprocessed by Frank Bub with raw data calculated over 1 m intervals, rather than smoothed over 5 m bins. The 5 m bins did not work well with inshore profiles. Negative numbers indicate instability. Use data with caution. </p> <p> Derived data are calculated using Matlab and/or UNH algorithms developed in accordance with standards prescribed by Fofonoff and Millard, 1983. </p> 10147 dye_bh dye_bh http://globec.whoi.edu/jg/serv/globec/gb/process/1999/dye_bh.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/dye_bh%7D <h2 align=center> Dye Experiment<br>Study of Cross-Frontal Exchange<br> R/V Oceanus Cruise 342</h2> <br> <b>DMO notes:</b><p> The documentation below describes a two ship operation. The data reported here are from the Bob Houghton cruise on the Oceanus 342.</p> <b>PI docmentation:</b><br> <p> Two cruises were undertaken in May and June 1999 in which dye patches were released to study cross-frontal exchange. On Oceanus Cruise 342, led by Bob Houghton of LDEO, dye was released in the bottom mixed layer. A Scanfish towed unit was used to moniter the dispersion of dye as well as locate the frontal system on the Southern flank of Georges Bank. Jim Ledwell and Jim Churchill of WHOI led Endeavor Cruise 323/324 in which dye and drifters were deployed in the pycnocline and in the surface layer. Sampling on this cruise was done by the WHOI VPR group, yielding plankton distributions. <p> <a href="http://globec.whoi.edu/globec-dir/reports/data_workshops/cross-frontal_exchange/cfe-ssc_report_2000/houghton_fig1mapcap.html"> Figure 1</a> shows the location of dye and drifter deployments during these cruises. The LDEO dye was Fluorescein injected into the bottom mixed layer on the stratified side of the tidal front. The WHOI dye was Rhodamine-WT: #1 injected into the surface (1-3 m ) layer and #2-4 into the pycnocline. During the WHOI dye injections additional WHOI drifters drogued at various depths were deployed in the dye patch. Drifters also drogued at various depths were deployed by Manning in April and May on NOAA cruises. See the time line for the temporal distribution of the experiments. <p> Additional information about this experiment is available at the on-line report entitled <a href="http://globec.whoi.edu/globec-dir/reports/data_workshops/cross-frontal_exchange/cfe-ssc_report_2000/distribution_of_salinity_on_the_cap.html"> Distribution of Salinity on the Cap of Georges Bank</a> <p> The work is described in more detail in the following cruise reports:<p> Houghton, R. W., R/V Oceanus Cruise 342 to Georges Bank, <a href="http://globec.whoi.edu/globec-dir/reports/oc342/oc342cruisereport.html">Cruise Report</a>, U. S. GLOBEC Northwest Atlantic/Georges Bank Program, 1999. <p> Ledwell, J. R., T. G. Donoghue, C. J. Sellers, J. H. Churchill, D. Torres, D. McGillicuddy, V. Kosnyrev, C. S. Davis, S. M. Gallager, C. J. Ashjian, A. P. Girard, P. Alatalo, and Q. Hu, Lagrangian Studies of the Tidal Mixing Front on Georges Bank, R/V Endeavor Cruises 323 and 324, <a href="http://globec.whoi.edu/globec-dir/reports/en323/globecnew.html">Cruise Report</a>, U. S. GLOBEC Northwest Atlantic/Georges Bank Program, 2000. <p> McGillicuddy, D. J., and V. K. Kosnyrev, Real-Time Modeling on Cruises EN323 and EN324, Cruise Report, U. S. GLOBEC Northwest Atlantic/Georges Bank Program, 1999. </p><br> <pre> <b>Questions concerning these data should be directed to:</b> Bob Houghton Lamont-Doherty Earth Observatory of Columbia Univ. 202 Oceanography Palisades, NY 10964 Phone: 845-365-8328 E-mail: <a href="mailto:houghton@ldeo.columbia.edu">houghton@ldeo.columbia.edu</a> <i>Last updated March 28, 2006</i> </pre> On Oceanus Cruise 342, led by Bob Houghton of LDEO, dye was released in the bottom mixed layer. A Scanfish towed unit was used to moniter the dispersion of dye as well as locate the frontal system on the Southern flank of Georges Bank. Jim Ledwell and Jim Churchill of WHOI led Endeavor Cruise 323/324 in which dye and drifters were deployed in the pycnocline and in the surface layer. Sampling on this cruise was done by the WHOI VPR group, yielding plankton distributions. </p><p> <a href="http://globec.whoi.edu/globec-dir/reports/data_workshops/cross-frontal_exchange/cfe-ssc_report_2000/houghton_fig1mapcap.html"> Figure 1</a> shows the location of dye and drifter deployments during these cruises. The LDEO dye was Fluorescein injected into the bottom mixed layer on the stratified side of the tidal front. The WHOI dye was Rhodamine-WT: #1 injected into the surface (1-3 m ) layer and #2-4 into the pycnocline. During the WHOI dye injections additional WHOI drifters drogued at various depths were deployed in the dye patch. Drifters also drogued at various depths were deployed by Manning in April and May on NOAA cruises. See the time line for the temporal distribution of the experiments. <p> Additional information about this experiment is available at the on-line report entitled <a href="http://globec.whoi.edu/globec-dir/reports/data_workshops/cross-frontal_exchange/cfe-ssc_report_2000/distribution_of_salinity_on_the_cap.html"> Distribution of Salinity on the Cap of Georges Bank</a> </p> 10148 epiflu epiflu http://globec.whoi.edu/jg/serv/globec/gb/process/epiflu.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/epiflu%7D <h3 align=center> EN321<br>Bacterial Cell Counts, Biovolumes and Biomass per taxon<br> from epifluorescence microscopy </h3> <pre> Submitted by: Michael Sieracki Bigelow Laboratory for Ocean Science McKown Pt. Road W. Boothbay Harbor, ME 04575 <a href="mailto:msieracki@bigelow.org">msieracki@bigelow.org</a> <i>updated: June 7, 2005, gfh </i></pre> EN321 Bacterial Cell Counts, Biovolumes and Biomass per taxon from epifluorescence microscopy 10149 eultide eultide http://globec.whoi.edu/jg/serv/globec/gb/process/eultide.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/eultide%7D <h3 align=center> Eulerian Tidal Data from 1999</h3> <P><font size="+2">T</font>he database is designed as a hierarchy. The least changing variables are in higher order tables (e.g., cruise id, year, etc.), while variables that change the most are in the lower order tables (e.g., bottle numbers, nutrient measured, etc.) There are three levels within the database; variable names and descriptions are given in the following tables. The information in the relational database is contained in the header at each level so that all relevant data is available at all levels. </P> <P><font size="+2">M</font>ost column variable names and instrument names were taken from the U.S. GLOBEC Georges Bank data thesaurus; those that were not follow the GLOBEC data protocols. </p> 10150 EN321fcmbact EN321fcmbact http://globec.whoi.edu/jg/serv/globec/gb/process/EN321fcmbact.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/EN321fcmbact%7D <h3 align=center> EN321 Bacteria counts from Flow Cytometer </h3> <pre> Submitted by: Michael Sieracki Bigelow Laboratory for Ocean Science McKown Pt. Road W. Boothbay Harbor, ME 04575 <a href="mailto:msieracki@bigelow.org">msieracki@bigelow.org</a> <i>updated: Sept 1, 2005, gfh </i></pre> EN321 Bacteria counts from Flow Cytometer 10151 EN321fcmnano EN321fcmnano http://globec.whoi.edu/jg/serv/globec/gb/process/EN321fcmnano.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/EN321fcmnano%7D <h3 align=center> Nanoplankton from Flow Cytometry</h3> <pre> Submitted by: Michael Sieracki Bigelow Laboratory for Ocean Science McKown Pt. Road W. Boothbay Harbor, ME 04575 <a href="mailto:msieracki@bigelow.org">msieracki@bigelow.org</a> <i>updated: Sept 13, 2006, gfh </i></pre> Nanoplankton from Flow Cytometry 10152 EN325fcmbact EN325fcmbact http://globec.whoi.edu/jg/serv/globec/gb/process/EN325fcmbact.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/EN325fcmbact%7D <h3 align=center> Bacteria counts from Flow Cytometer </h3> <pre> Submitted by: Michael Sieracki Bigelow Laboratory for Ocean Science McKown Pt. Road W. Boothbay Harbor, ME 04575 <a href="mailto:msieracki@bigelow.org">msieracki@bigelow.org</a> <i>updated: Sept 1, 2005, gfh </i></pre> Bacteria counts from Flow Cytometer 10153 microstructs06 microstructs06 http://globec.whoi.edu/jg/serv/globec/gb/process/1995/S06_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/microstructs06%7D <h2 align=center> Averages of EPSONDE Microstructure Profiles</h2> <h2 align=center> Shallow Site, Seward Johnson 95-06</h2> <p> Typically, an EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. <p> <b>DMO Note:</b> This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. <pre> Prepared by: Russ Burgett, University of Rhode Island, GSO Reference: (S06 - GL1AVG) </pre> <p> Details of data processing are described in: U.S. GLOBEC Georges Bank microsturcture data. GSO Univ. Rhode Island Tech. report 96-6. <pre> <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 phone: 401 874 6610 fax: 401 874 6728 e-mail: <a href="mailto:david.hebert@gso.uri.edu">david.hebert@gso.uri.edu<a> <i>Updated: September 10, 2004; gfh</i></pre> Typically, an EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. 10154 microstructd06 microstructd06 http://globec.whoi.edu/jg/serv/globec/gb/process/1995/D06_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/microstructd06%7D <h2 align=center> Averages of EPSONDE Microstructure Profiles</h2> <h2 align=center> Deep Site, Seward Johnson 95-06</h2> <p> Typically, an EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. <p> <b>DMO Note:</b> This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. <pre> Prepared by: Russ Burgett, University of Rhode Island, GSO Reference: (D06 - GL2AVG) </pre> <p> Details of data processing are described in: U.S. GLOBEC Georges Bank microsturcture data. GSO Univ. Rhode Island Tech. report 96-6. <pre> <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 phone: 401 874 6610 fax: 401 874 6728 e-mail: <a href="mailto:david.hebert@gso.uri.edu">david.hebert@gso.uri.edu<a> <i>Updated: September 10, 2004; G.Heimerdinger</i></pre> EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. 10155 microstructs08 microstructs08 http://globec.whoi.edu/jg/serv/globec/gb/process/1995/S08_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/microstructs08%7D <h2 align=center> Averages of EPSONDE Microstructure Profiles</h2> <h2 align=center> Shallow Site, Seward Johnson 95-08</h2> <p> Typically, an EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. <p> <b>DMO Note:</b> This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. <pre> Prepared by: Russ Burgett, University of Rhode Island, GSO Reference: (S08 - GS1AVG) </pre> <p> Details of data processing are described in: U.S. GLOBEC Georges Bank microsturcture data. GSO Univ. Rhode Island Tech. report 96-6. <pre> <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 phone: 401 874 6610 fax: 401 874 6728 e-mail: <a href="mailto:david.hebert@gso.uri.edu">david.hebert@gso.uri.edu<a> <i>Updated: September 10, 2004; gfh</i></pre> EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles per profile number. This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. 10156 microstructd08 microstructd08 http://globec.whoi.edu/jg/serv/globec/gb/process/1995/D08_rs.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/microstructd08%7D <h2 align=center> Averages of EPSONDE Microstructure Profiles</h2> <h2 align=center> Deep Site, Seward Johnson 95-08</h2> <p> Typically, an EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles for each profile number. <p> <b>DMO Note:</b> This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. <pre> Prepared by: Russ Burgett, University of Rhode Island, GSO Reference: (D08 - GS2AVG) </pre> <p> Details of data processing are described in: U.S. GLOBEC Georges Bank microsturcture data. GSO Univ. Rhode Island Tech. report 96-6. <pre> <b>Contributor:</b> Dave Hebert Graduate School of Oceanography Univ. of Rhode Island Narragansett, RI 02882-1197 phone: 401 874 6610 fax: 401 874 6728 e-mail: <a href="mailto:david.hebert@gso.uri.edu">david.hebert@gso.uri.edu<a> <i>Updated: September 10, 2004; gfh</i></pre> EPSONDE microstructure profile is the average of 10 deployments of the EPSONDE instrument. One microstructure profile per profile number. During Seward Johnson cruise SJ9508, 20 deployments were made during each sampling event resulting in 2 microstructure profiles for each profile number. This data set as submitted contained the parameter "station". In the context of our definition, station was used incorrectly. We have changed this parameter to "profile" with the definition of: consecutively numbered averaged EPSONDE profile. Users consulting the GSO Tech. Report should equate profile number with station number. 10157 nmfs_ctdsb nmfs_ctdsb http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/nmfs_ctdsb.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/nmfs_ctdsb%7D <pre> PI: Jim Manning Dataset: SEABIRD 911 CTD data Ship: R/V OCEANUS Cruise(s): 301,303 <b>Data submitted by:</b> James Manning National Marine Fisheries Service, NEFC Woods Hole, MA 02543 voice: 508-495-2000 fax: 508-495-2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> </pre> <i>prepared by: Jim Manning, NMFS/Woods Hole Updated: 26 Feb. 2004, gfh </i> </pre> <pre> SEABIRD 9/11 CTD cast They are calibrated with Niskin bottles but a salt correction was not applied (<0.01 psu mean difference). ottles </pre> 10158 nmfs_drift nmfs_drift http://jgof.wh.whoi.edu/jg/serv/globec/gb/process/nmfs_drift.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/nmfs_drift%7D <h2 align=center>Small scale surface drifters</h2> <p> <pre> <b>Contributors:</b> Jim Manning National Marine Fisheries Service, NEFC Woods Hole, MA 02543 voice: 508-495-2211 fax: 508-495-2258 email: <a href="mailto:jmanning@whsun1.wh.whoi.edu">jmanning@whsun1.wh.whoi.edu</a> Jim Churchill Woods Hole Oceanographic Institution Woods Hole, MA 02543 <i>Updated: August 2, 2004, gfh </i></pre> Georges Bank GPS/ARGOS/VHF drifter data 10159 seasoar_ctd seasoar_ctd http://globec.whoi.edu/jg/serv/globec/gb/process/1999/seasoar_ctd.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/seasoar_ctd%7D The seasoar is a towed, undulating vehicle which records CTD and other data. The system records SeaBird CTD data at 24 hz, and it had other sensors on the A/D channels. The seasoar gets towed along different tracklines to map out various survey areas. Each time the seasoar is deployed and recovered is one "tow", and each of the cruises have a number of tows. <p> <pre> PI: Jack Barth (OSU), Dave Hebert (URI) dataset: SeaSoar CTD data project/cruise: R/V Oceanus Cruise 340 and 343 to Georges Bank ship: Oceanus Cruise details given in: Hebert, D., J. A. Barth, D. Ullman, S. Fontana and W. Ostrom, 1999. Cruise Report: R/V Oceanus Cruise 340 to Georges Bank, 28 March to 12 April 1999. US GLOBEC NW Atlantic/Georges Bank Study, 37 pp. Methods are described in: SeaSoar CTD Observations During the Coastal Mixing and Optics Experiment: R/V Endeavor Cruises from 14-Aug to 1-Sep 1996 and 25-Apr to 15-May 1997. R. O'Malley, J.A. Barth, A. Erofeev, J. Fleischbein, P.M. Kosro and S.D. Pierce. College of Oceanic & Atmospheric Sciences, Oregon State University, Corvallis. Reference 98-1, Data Report 168, October 1998. Hebert, D., J. A. Barth, D. Ullman and S. Fontana, 1999. Cruise Report: R/V Oceanus Cruise 343 to Georges Bank, 14 June to 1 July 1999. US GLOBEC NW Atlantic/Georges Bank Study, 40 pp. These are flat files, with data every 1-sec for each tow. The tows are numbered sequentialy (tow1, tow2, etc). </pre> <p> <b>Notes: </b><br> 1. There are two fields for different fluorometers: flvolt (aka FL-1) is from a WetLabs Wetstar fluorometer, while flvolt_2 (aka FL-2) is from a WetLabs FlashPAK fluorometer. <p> 2. Original field name is shown in parenthesis in the "Description" column. <p> 3. There were some problems in the data fields whenever the lat/lon were interpolated for lack of GPS observations. The OC343 data files were replaced on-line with the reprocessed files October 16, 2000. <p> </pre> The seasoar is a towed, undulating vehicle which records CTD and other data. The system records SeaBird CTD data at 24 hz, and it had other sensors on the A/D channels. The seasoar gets towed along different tracklines to map out various survey areas. Each time the seasoar is deployed and recovered is one &#039;tow&#039;, and each of the cruises have a number of tows. <pre> Methods are described in: SeaSoar CTD Observations During the Coastal Mixing and Optics Experiment: R/V Endeavor Cruises from 14-Aug to 1-Sep 1996 and 25-Apr to 15-May 1997. R. O&#039;Malley, J.A. Barth, A. Erofeev, J. Fleischbein, P.M. Kosro and S.D. Pierce. College of Oceanic &amp; Atmospheric Sciences, Oregon State University, Corvallis. Reference 98-1, Data Report 168, October 1998. Hebert, D., J. A. Barth, D. Ullman and S. Fontana, 1999. Cruise Report: R/V Oceanus Cruise 343 to Georges Bank, 14 June to 1 July 1999. US GLOBEC NW Atlantic/Georges Bank Study, 40 pp. These are flat files, with data every 1-sec for each tow. The tows are numbered sequentialy (tow1, tow2, etc). </pre> 10160 scanfish scanfish http://globec.whoi.edu/jg/serv/globec/gb/process/1999/scanfish.brev0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/process/,info=globec.whoi.edu/jg/info/globec/gb/process/scanfish%7D <h2 align=center> SCANFISH CTD Data <br> Endeavor Cruises 321 and 325</H2> <p> <b>PI Notes: </b><br> The Scanfish is a towed undulating vehicle carrying a CTD and several other sensors and was utilized on Endeavor Cruises 321 and 325 to Georges Bank. The scanfish is towed along various transacts to map the hydrographic properties of a survey area. During each cruise a number of tows were carried out, and the data are organized by tow. The SeaBird 911plus CTD records data at 24 Hz. It has been processed following the procedures outlined by O'Malley, et al (1998) and subsequently averaged to 1 Hz. <br><br> <b>REFERENCE</b><br> O'Malley, R., J. A. Barth, A. Erofeev, J. Fleischbein, P. M. Kosro, and S. D. Pierce. SeaSoar CTD Observations During the Coastal Mixing and Optics Experiment: R/V Endeavor Cruises from 14-Aug to 1-Sep 1996 and 25-Apr to 15-May 1997. College of Oceanic & Atmospheric Sciences, Oregon State University, Corvallis. Reference 98-1, Data Report 168, October 1998. </p><pre> <b>Questions regarding these data should be directed to: </b> Dian J. Gifford Graduate School of Oceanography University of Rhode Island Narragansett, RI 02882-1197 phone: 401-874-6690 fax: 401-874-6240 E-mail: <a href="mailto:gifford@gsosun1.gso.uri.edu">gifford@gsosun1.gso.uri.edu</a> or Karen Wishner Graduate School of Oceanography University of Rhode Island Narragansett, RI 02882-1197 phone: 401-874-6402 E-mail: <a href="mailto: kwishner@gsosun1.gso.uri.edu">kwishner@gsosun1.gso.uri.edu</a> <i>Last updated, March 24, 2006, gfh</i> </pre> The Scanfish is a towed undulating vehicle carrying a CTD and several other sensors and was utilized on Endeavor Cruises 321 and 325 to Georges Bank. The scanfish is towed along various transacts to map the hydrographic properties of a survey area. During each cruise a number of tows were carried out, and the data are organized by tow. The SeaBird 911plus CTD records data at 24 Hz. It has been processed following the procedures outlined by O&#039;Malley, et al (1998) and subsequently averaged to 1 Hz. 10161 1993_avhrr 1993_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1993.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1993_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10162 1994_avhrr 1994_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1994.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1994_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10163 1995_avhrr 1995_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1995.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1995_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10164 1996_avhrr 1996_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1996.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1996_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10165 1997_avhrr 1997_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1997.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1997_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10166 1998_avhrr 1998_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1998.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1998_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10167 1999_avhrr 1999_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_1999.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/1999_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10168 2000_avhrr 2000_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_2000.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/2000_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10169 2001_avhrr 2001_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_2001.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/2001_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10170 2002_avhrr 2002_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_2002.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/2002_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10171 2003_avhrr 2003_avhrr http://rodan.cmast.umassd.edu/jg/serv/globec/gb/satellite/avhrr_2003.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/2003_avhrr%7D <h4> PI: J. J. Bisagni<br> Dataset: Satellite-derived AVHRR SST images </h4> <h4>AVHRR SST Images</h4> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain,<p> 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude,</p><p> 1 October 1993 - 2003. </p><h4> Data Provider</h4> <address> </address><dir> Dr. J. J. Bisagni<br> Center for Marine Science and Technology <br> University of Massachusetts <br> 285 Old Westport Road <br> North Dartmouth, MA 02747 <br> 508-999-8359 <br> jbisagni@umassd.edu <br> FAX: 508-999-8197<br> </dir> <h4>Summary of Satellites Availabe, by Year</h4> <p> <table border="1"> <tbody><tr><th>Year</th> <th>Satellite</th></tr> <tr><td>1993</td> <td>NOAA-11</td></tr> <tr><td>1994</td> <td>NOAA-11 (January - September), NOAA-9 (September - December)</td></tr> <tr><td>1995</td> <td>NOAA-11, NOAA-9</td></tr> <tr><td>1996</td> <td>NOAA-14</td></tr> <tr><td>1997</td> <td>NOAA-14</td></tr> <tr><td>1998</td> <td>NOAA-14</td></tr> <tr><td>1999</td> <td>NOAA-14, NOAA-15 (starting in December)</td></tr> <tr><td>2000</td> <td>NOAA-14, NOAA-15 (January - July), NOAA-16 (October - December)</td></tr> <tr><td>2001</td> <td>NOAA-14 (mostly bad, use NOAA-15), NOAA-15 (October - December), NOAA-16</td></tr> <tr><td>2002</td> <td>NOAA-14 (still mostly bad, use NOAA-15), NOAA-15, NOAA-16</td></tr> </tbody></table> </p><h4> Notes</h4> <ul> <li>The image aspect ratio is now correct. The images should be square. This problem within the IDL engine was solved November 2007 by switching to the ferret application to generate the images.</li> <li>Images are 512 X 512 pixels, possess a resolution of 1.4 km and are displayed as .GIF images.</li> <li>The archive "switches" from NOAA-11 to NOAA-9 during September 1994 due to the NOAA-11 failure in September 1994.</li> <li>Starting in 1994, all NOAA-9, -12 and -14 overpasses are remapped to the above domain and added to the archive on a daily basis.</li> <li>At the end of each month, all the month's images are precision navigated to within 1-2 pixels (1.4-2.8 km). NOAA-12 and -14 data are then saved to tape and deleted, due to calibration problems with NOAA-12 and -14 and to conserve disk space.</li> <li>During the initial data acquisition time, images from the current month may possessed navigation errors of up to 3-5 pixels or more in the X and/or Y directions.</li> <li>Starting August 2002, images from NOAA-17 ("b") became available. They seem to have replaced the NOAA-14 ("f") images.</li> <li>The colorbar used is derived from so-called Pete's Palette, or pete24, and converted to an equivalent palette in the ferret scheme. (See <a href="http://globec.whoi.edu/globec-dir/data_doc/petespalette.txt" target="_blank"> petespalette.spk</a>. </li></ul> <h4> Additional Information About Image Processing</h4> <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projection. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the ferret application for display by your favorite browser, such as Internet Explorer, Mozilla, and Firefox. </p><h4> XBrowse Software </h4> <p>Near real-time, daily, satellite-derived sea surface temperature (SST) data, which cover Georges Bank and the Gulf of Maine are also available for browsing over the Internet in the Xbrowse format. This browse capability is being made available via the Xbrowse (X-window based) client/server system developed by Jim Gallagher (jimg@dcz.gso.uri.edu) in Peter Cornillon's group located at the University of Rhode Island's Graduate School of Oceanography. In addition to visual "browsing" of the data, the Xbrowse system also allows the names of user-selected images to be listed in a file on your local host for later use in retrieving those images from the Xbrowse server via ftp. <a href="http://dcz.gso.uri.edu/avhrr-archive/archive.html" target="_blank"> http://dcz.gso.uri.edu/avhrr-archive/archive.html</a> </p><p>The latest Xbrowse client (ver. 3.3.7) and accessory files used to be available for SunOS 4.1.3 (Sun SPARC), OSF 1.3 (DEC Alpha) and Ultrix 4.3 (DECstation) via anonymous ftp from zeno.gso.uri.edu (/pub/xbrowse) and had to be uncompressed, restored (via "tar") and properly installed on your local host for the system to work. You might be able to get help by contacting the datamaster at GSO/URI at <a href="mailto:datamaster@mail.po.gso.uri.edu">datamaster@mail.po.gso.uri.edu</a>. </p><p>Assuming that the client is properly installed on your local host, you can start the remote server by typing: <b>xbrowse -server dcz.gso.uri.edu </b> </p><p>Those of you who have an earlier version of Xbrowse and would like access to the server should get an update because the latest version handles the Mercator projection properly. </p><h4>DODS System</h4> These images are also viewable via <a href="http://www.unidata.ucar.edu/packages/dods/">DODS, Distributed Oceanographic Data System</a>. <h4>Downloading the image</h4> <p>You can capture the gif image if your browser has that capability. In addition, if you would like to download any of the Xbrowse images over the network to your local host for your own use, please <a href="mailto:jbisagni@umassd.edu">contact me</a> directly. </p><p> </p><hr> <i>Last edited: November 14, 2007</i> Satellite-derived AVHRR SST images for the US-GLOBEC Georges Bank Program study domain, 39.013 - 45.429 degree North latitude, 63.487 - 72.164 degree West longitude, 1 October 1993 - present day. <p>At the present time all daily NOAA-11 Advanced Very High Resolution Radiometer satellite passes from 1 October 1993 on (generally 2 passes per day) have been remapped (earth-located) to our Georges Bank/Gulf of Maine "standard" region (given below) in a Mercator projectio. Our standard region is bounded by: </p><ul> <li>39.013 - 45.429 degree North latitude, and </li> <li>63.487 - 72.164 degree West longitude.</li> </ul> <p>Precision navigation of each image to within 1 or 2 pixels has begun with the image file names receiving a ".nav" file extension when navigation is completed. Be aware that "un- navigated" images (".rmp" file extension) may possess navigation errors of up to 6 or 7 pixels in the meridional and/or zonal directions. Note that only ".nav" files are being served here at this time. </p><p>Daily remapping and weekly backups of these data will continue until after completion of the GLOBEC and Gulf of Maine field programs are completed. Each of these images are in University of Miami XDR04 format, consisting of an 8-bit, 512 X 512 pixel binary image, preceded by three 512-byte header records. The size of each image file (in uncompressed form) is ~250K bytes. </p><p>These images are uncompressed and converted from Xbrowse to gif images via the DODS and IDS systems for display by your favorite browser, such as Internet Explorer or Netscape. 10172 gs_rings gs_rings http://globec.whoi.edu/jg/serv/globec/gb/satellite/gs_rings.html0%7Bdir=globec.whoi.edu/jg/dir/globec/gb/satellite/,info=globec.whoi.edu/jg/info/globec/gb/satellite/gs_rings%7D <pre> <html xmlns:v="urn:schemas-microsoft-com:vml" xmlns:o="urn:schemas-microsoft-com:office:office" xmlns:w="urn:schemas-microsoft-com:office:word" xmlns:x="urn:schemas-microsoft-com:office:excel" xmlns="http://www.w3.org/TR/REC-html40"> </pre> <head> <meta http-equiv=Content-Type content="text/html; charset=windows-1252"> <meta name=ProgId content=Word.Document> <meta name=Generator content="Microsoft Word 9"> <meta name=Originator content="Microsoft Word 9"> <link rel=File-List href="./filelist.xml"> <link rel=Edit-Time-Data href="./editdata.mso"> <!--[if !mso]> <style> v:* {behavior:url(#default#VML);} o:* {behavior:url(#default#VML);} w:* {behavior:url(#default#VML);} .shape {behavior:url(#default#VML);} </style> <![endif]--> <title>Yearly Animations of Northwest Atlantic Surface Temperature Showing the Interaction of Gulf Stream Rings and Meanders with the</title> <!--[if gte mso 9]><xml> <o:DocumentProperties> <o:Author>Richard</o:Author> <o:LastAuthor>Richard</o:LastAuthor> <o:Revision>2</o:Revision> <o:TotalTime>11</o:TotalTime> <o:Created>2000-02-18T20:30:00Z</o:Created> <o:LastSaved>2000-02-18T20:30:00Z</o:LastSaved> <o:Pages>3</o:Pages> <o:Words>474</o:Words> <o:Characters>2703</o:Characters> <o:Company>Limeburner</o:Company> <o:Lines>22</o:Lines> <o:Paragraphs>5</o:Paragraphs> <o:CharactersWithSpaces>3319</o:CharactersWithSpaces> <o:Version>9.2720</o:Version> </o:DocumentProperties> </xml><![endif]--> <style> <!-- /* Style Definitions */ p.MsoNormal, li.MsoNormal, div.MsoNormal {mso-style-parent:""; 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The objective of this effort was to document the times when Gulf Stream rings entrained shelf water and/or intruded slope water onto the shelf<span style="mso-spacerun: yes"> </span>near Georges Bank and Browns Bank.</p> <p class='MsoNormal' style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>The animations are in a flc format and require a player. Sources of free players are available from <a href="http://www.gromada.com/index.html">http://www.gromada.com/index.html</a> (the Moyager PC player) and <a href="http://globec.whoi.edu/globec-dir/aaplay.html">http://globec.whoi.edu/globec-dir/aaplay.html</a>. In the near future these animations will automatically play over the Internet without installing the players. </p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>The JHUAPL SST data archives begin December 1996 for the Gulf Stream region and the yearly animations are named <a href="http://globec.whoi.edu/globec-dir/gulf_stream_rings/sst99.flc">sst97.flc</a>, <a href="http://globec.whoi.edu/globec-dir/gulf_stream_rings/sst99.flc">sst98.flc</a>, and <a href="http://globec.whoi.edu/globec-dir/gulf_stream_rings/sst99.flc">sst99.flc</a>. The 60-m and 200-m isobaths were laid over the SST imagery and a time stamp was added. The date of each SST image corresponds to the center of a 3-day window of images that were made into a composite image.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>The monthly locations of Gulf Stream rings was located in the animations and plotted below for each year. Note the anomalously high number of rings in 1999.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><!--[if gte vml 1]><v:shapetype id="_x0000_t75" coordsize="21600,21600" o:spt="75" o:preferrelative="t" path="m@4@5l@4@11@9@11@9@5xe" filled="f" stroked="f"> <v:stroke joinstyle="miter"/> <v:formulas> <v:f eqn="if lineDrawn pixelLineWidth 0"/> <v:f eqn="sum @0 1 0"/> <v:f eqn="sum 0 0 @1"/> <v:f eqn="prod @2 1 2"/> <v:f eqn="prod @3 21600 pixelWidth"/> <v:f eqn="prod @3 21600 pixelHeight"/> <v:f eqn="sum @0 0 1"/> <v:f eqn="prod @6 1 2"/> <v:f eqn="prod @7 21600 pixelWidth"/> <v:f eqn="sum @8 21600 0"/> <v:f eqn="prod @7 21600 pixelHeight"/> <v:f eqn="sum @10 21600 0"/> </v:formulas> <v:path o:extrusionok="f" gradientshapeok="t" o:connecttype="rect"/> <o:lock v:ext="edit" aspectratio="t"/> </v:shapetype><v:shape id="_x0000_i1028" type="#_x0000_t75" style='width:6in; height:324pt'> <v:imagedata src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image001.png" o:title="map97rings"/> </v:shape><![endif]--><![if !vml]><img border=0 width=576 height=432 src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image002.jpg" alt="MATLAB Handle Graphics" v:shapes="_x0000_i1028"><![endif]></p> <p class=MsoNormal style='text-indent:.5in'>Figure 1. 1997 monthly ring positions.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><!--[if gte vml 1]><v:shape id="_x0000_i1029" type="#_x0000_t75" style='width:6in;height:324pt'> <v:imagedata src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image003.png" o:title="map98rings"/> </v:shape><![endif]--><![if !vml]><img border=0 width=576 height=432 src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image004.jpg" alt="MATLAB Handle Graphics" v:shapes="_x0000_i1029"><![endif]></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>Figure 2. 1998 monthly ring positions.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><!--[if gte vml 1]><v:shape id="_x0000_i1030" type="#_x0000_t75" style='width:6in;height:324pt'> <v:imagedata src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image005.png" o:title="map99rings"/> </v:shape><![endif]--><![if !vml]><img border=0 width=576 height=432 src="http://globec.whoi.edu/globec-dir/gulf_stream_rings/image006.jpg" alt="MATLAB Handle Graphics" v:shapes="_x0000_i1030"><![endif]></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>Figure 3. 1999 monthly ring positions.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal>The presence of GS Ring Water R and Warm Slope Water S north of the 200-m isobath on the south side of Georges Bank is show for 1997 (Table 1), 1998 (Table 2), and 1999 (Table 3).</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <table border=0 cellspacing=0 cellpadding=0 style='border-collapse:collapse; mso-padding-alt:0in 1.5pt 0in 1.5pt'> <tr style='height:13.8pt'> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal style='mso-layout-grid-align:none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial;color:black'>Longitude<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Dec-96<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Jan-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Feb-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Mar-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Apr-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>May-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Jun-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Jul-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Aug-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Sep-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Oct-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Nov-97<o:p></o:p></span></b></p> </td> <td valign=top style='border:none;border-bottom:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.8pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>Dec-97<o:p></o:p></span></b></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-72<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class='MsoNormal' align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class="MsoNormal" align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-71<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-70<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-69<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-68<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'><span style="mso-spacerun: yes"> </span><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-67<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-66<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-65<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-64<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-63<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> <tr style='height:13.1pt'> <td valign=top style='border:none;border-right:solid windowtext 1.5pt; padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=right style='text-align:right;mso-layout-grid-align: none;text-autospace:none'><b><span style='font-size:10.0pt;font-family:Arial; color:black'>-62<o:p></o:p></span></b></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>S<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><span style='font-size:10.0pt;font-family:Arial; color:black'>R<o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> <td valign=top style='padding:0in 1.5pt 0in 1.5pt;height:13.1pt'> <p class=MsoNormal align=center style='text-align:center;mso-layout-grid-align: none;text-autospace:none'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial;color:black'><o:p></o:p></span></p> </td> </tr> </table> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>Table 1. Rings and slope water on shelf in 1997.</p> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <table border=0 cellspacing=0 cellpadding=0 width="100%" style='width:100.0%; border-collapse:collapse;mso-padding-alt:0in 0in 0in 0in'> <tr style='height:13.5pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal><b><span style='font-size:10.0pt;font-family:Arial'>Longitude<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Dec-96<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jan-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Feb-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Mar-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Apr-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>May-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jun-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jul-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Aug-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Sep-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Oct-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Nov-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;border:none;border-bottom: solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Dec-97<o:p></o:p></span></b></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-72<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-71<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-70<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-69<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-68<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-67<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-66<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-65<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-64<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-63<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="7%" nowrap valign=bottom style='width:7.82%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-62<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.1%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> </table> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'>Table 2. Rings and slope water on shelf in 1998.</p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <p class=MsoNormal style='text-indent:.5in'><![if !supportEmptyParas]> <![endif]><o:p></o:p></p> <table border=0 cellspacing=0 cellpadding=0 width="100%" style='width:100.0%; border-collapse:collapse;mso-padding-alt:0in 0in 0in 0in'> <tr style='height:13.5pt'> <td width="8%" nowrap valign=bottom style='width:8.42%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal><b><span style='font-size:10.0pt;font-family:Arial'>Longitude<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jan-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Feb-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Mar-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Apr-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>May-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jun-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Jul-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Aug-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Sep-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Oct-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Nov-97<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;border:none; border-bottom:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt; height:13.5pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>Dec-97<o:p></o:p></span></b></p> </td> </tr> <tr style='height:12.75pt'> <td width="8%" nowrap valign=bottom style='width:8.42%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-72<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><b><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="8%" nowrap valign=bottom style='width:8.42%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-71<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="8%" nowrap valign=bottom style='width:8.42%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-70<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>S<o:p></o:p></span></p> </td> </tr> <tr style='height:12.75pt'> <td width="8%" nowrap valign=bottom style='width:8.42%;border:none; border-right:solid windowtext 1.0pt;padding:.75pt .75pt 0in .75pt;height: 12.75pt'> <p class=MsoNormal align=right style='text-align:right'><b><span style='font-size:10.0pt;font-family:Arial'>-69<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><![if !supportEmptyParas]> <![endif]><span style='font-size:10.0pt;font-family:Arial'><o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; height:12.75pt'> <p class=MsoNormal align=center style='text-align:center'><b><span style='font-size:10.0pt;font-family:Arial'>R<o:p></o:p></span></b></p> </td> <td width="7%" nowrap valign=bottom style='width:7.64%;padding:.75pt .75pt 0in .75pt; 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