19:I[42426,["/_next/static/immutable/chunks/1xctgzqre-wsy.js","/_next/static/immutable/chunks/06_-wz6pdtp2b.js","/_next/static/immutable/chunks/30e52g49hg40p.js","/_next/static/immutable/chunks/02yq6tul2z-oh.js","/_next/static/immutable/chunks/10bx_ec2vj7n_.js","/_next/static/immutable/chunks/33bfn03fo8xnt.js","/_next/static/immutable/chunks/0tfjf78scu61b.js","/_next/static/immutable/chunks/31xnvej4n1bi9.js"],"default"] 1a:T6c1,

Example SeaSave processing, from cast 005.01:
# datcnv_date = Aug 28 2015 08:22:28, 7.23.2 [datcnv_vars = 17]
# datcnv_in = C:\Users\Tech\Desktop\Seasave\Raw\CTD_2015\BH15-11\005.01.hex C:\Users\Tech\Desktop\Seasave\Raw\CTD_2015\BH15-11\005.01.XMLCON
# datcnv_skipover = 0
# datcnv_ox_hysteresis_correction = yes
# datcnv_ox_tau_correction = yes
# filter_date = Aug 28 2015 08:23:15, 7.23.2
# filter_in = C:\Users\Tech\Desktop\Seasave\Converted Data\005.01.cnv
# filter_low_pass_tc_A = 0.150
# filter_low_pass_tc_B = 0.150
# filter_low_pass_A_vars = prDM
# filter_low_pass_B_vars =
# loopedit_date = Aug 28 2015 08:26:05, 7.23.2
# loopedit_in = C:\Users\Tech\Desktop\Seasave\Filter\005.01f.cnv
# loopedit_minVelocity = 0.100
# loopedit_surfaceSoak: do not remove
# loopedit_excl_bad_scans = yes
# binavg_date = Aug 28 2015 08:26:48, 7.23.2
# binavg_in = C:\Users\Tech\Desktop\Seasave\Loop Edit\005.01fle.cnv
# binavg_bintype = meters
# binavg_binsize = 1
# binavg_excl_bad_scans = yes
# binavg_skipover = 0
# binavg_surface_bin = no, min = 0.000, max = 0.000, value = 0.000
# file_type = ascii

BCO-DMO Processing Notes:
- Modified parameters names to conform with BCO-DMO naming conventions;
- Created ISO_DateTime field from dates in CTD .hdr files;
- Added column for "station_name".

1b:T527,NSF Award Abstract: This proposal to fund a research training cruise on the University of Minnesota's R/V Blue Heron for early career scientists from the Great Lakes basin. The proposed work will have two goals: 1) teach early career lacustrine scientists how to acquire, plan for, and manage cruises aboard UNOLS ships, possibly having some impact on the long-term decrease in requests for ship time on UNOLS ships in general; and 2) expose members of the Great Lakes scientific community, which has an abysmally low submittal rate of proposals to NSF requesting UNOLS ships, to UNOLS and the academic fleet. This project mirrors the successful Chief Scientist training program that Dr. Claire Reimers at Oregon State University has run on ocean-going ships such as the R/V Wecoma, New Horizon and Endeavor. Intellectual Merit : The training cruise envisioned herein will allow early career scientists to collect seed data and test hypotheses for future proposals to NSF. Broader Impacts : This proposal intends to educate the next generation of researchers about the capabilities of UNOLS. This type of outreach between UNOLS and potential users is not only important for the broader scientific community, but doubly important for the Great Lakes community which seems resistant to using assets like the UNOLS fleet.1c:T916,NSF Award Abstract: Human observations of Earth's climate span only a narrow window of Earth History. Understanding how and why Earth's climate changed before human observations can be overcome through the measurement and interpretation of the chemical composition of marine sediments. Accurate interpretation of these records -- also known as "proxy" records, because they stand in for direct measurements of environmental conditions in the past -- first requires that the behavior of the proxy be properly calibrated against direct observations in modern environments. This project will develop a novel proxy for marine nutrient utilization based on a comprehensive characterization of the chemical composition of particulate organic matter in the Southern Ocean. The formation and export of organic matter in the ocean requires nutrients, consumes carbon, and can influence the global air-sea balance of carbon dioxide. New proxies and calibrations offer novel ways of looking at Earth's climate history and can potentially illuminate interactions within marine ecosystems. The efficiency of the biological carbon pump depends critically on the availability and utilization of marine nutrients, particularly in the Southern Ocean. However, ambiguity in, and disagreement between current nutrient utilization paleoproxies renders reconstruction of past nutrient regimes uncertain. Cadmium -- a known proxy for phosphate -- offers a means to circumvent many of the known limitations of existing nutrient proxies, but requires a full isotopic characterization before its application. In this project, researchers will trace the stable isotopic composition of cadmium recorded in organic matter using multiple collector inductively coupled plasma mass spectrometry. The researchers will make isotopic measurements across numerous surface nutrient regimes in the Southern Ocean, with a focus on three critical geochemical transitions: the formation of organic carbon at the sea surface, its transit and decomposition through the ocean's interior, and its behavior during burial on the sea floor. This sea surface-to-sea floor calibration will thus comprehensively determine the utility and fidelity of a novel nutrient proxy, allowing a more accurate view of how Earth's climate was related to ocean biogeochemistry in the past.6:["$","$L19",null,{"dataset":{"_id":"708293","description":"

Processed CTD data from BH15-11.

Related publications:Horner, T. J., Pryer, H. V., Nielsen, S. G., Crockford, P. W., Gauglitz, J. M., Wing, B. A., & Ricketts, R. D. (2017). Pelagic barite precipitation at micromolar ambient sulfate. Nature Communications, 8(1). doi:10.1038/s41467-017-01229-5

\n","problem":"","acquisition":"

CTD casts were conducted using using a Sea-Bird SBE 9 and SBE 11plus V 5.0. The CTD rosette included: WET Labs WETstar, SBE43 (oxygen), WET Labs CDOM, WET Labs C-Star, and Biospherical/Licor sensors. Data were processed (data conversion, filter, loop edit, bin average, ascii out) using Seasave V 7.23.2.

Notes:
\n- These data include both the up and down cast at each station. Because Niskin bottles were fired at certain depths on the upcasts, \"nbin\" values may be very high at those depths (because the CTD sat at depth for a longer period of time).
\n- Cast 002.01 was aborted due to a transmissometer issue.

Also see: Cast logs from cruise BH15-11 (PDF).

\n","processing":"$1a","bcodmoProcessing":"","title":"Processed CTD data from BH15-11 from R/V Blue Heron cruise BH15-11 in the western arm of Lake Superior in August 2015","nickname":"BH15-11 CTD","dataUrl":"","currentState":"Final no updates expected","currentStateId":"7","validated":true,"restricted":false,"version":"1","version_date":"2017-07-20T04:00:00.000Z","abstract":"Processed CTD data from BH15-11 from R/V Blue Heron cruise BH15-11 in the western arm of Lake Superior in August 2015.","citation":"Horner, T. (2017) Processed CTD data from BH15-11 from R/V Blue Heron cruise BH15-11 in the western arm of Lake Superior in August 2015. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2017-07-20 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.708293.1 [access date]","citationParts":{"identifier":"doi:10.1575/1912/bco-dmo.708293.1","versionDate":"2017-07-20","versionId":"1","year":"2017","title":"Processed CTD data from BH15-11 from R/V Blue Heron cruise BH15-11 in the western arm of Lake Superior in August 2015","authors":"Horner, T.","publisher":"Biological and Chemical Oceanography Data Management Office (BCO-DMO)."},"doi":"10.1575/1912/bco-dmo.708293.1","release_date":null,"field_dataset_location":"","temporal_extent":{"start":"2015-08-26T04:00:00.000Z","end":"2015-08-28T04:00:00.000Z"},"temporal":{"resolution":"time:unitDay","type":"time:Interval","start":{"value":"1440561600","label":"2015-08-26"},"end":{"value":"1440734400","label":"2015-08-28"}},"spatial_extent":{"shape":"polygon","center":{"latitude":47.041100000006,"longitude":-90.883250000012},"wkt":"POLYGON ((-91.9442 46.7502, -89.8223 46.7502, -89.8223 47.332, -91.9442 47.332, -91.9442 46.7502))","north":47.332,"east":-89.8223,"south":46.7502,"west":-91.9442},"dataset_type":["Cruise Results"],"keywords":["oceans"],"data_files":[{"id":"901678","title":"ctd_BH1511.csv","url":"https://datadocs.bco-dmo.org/dataset/708293/file/JEE1Mq9Hyl9Ygj/ctd_BH1511.csv","showTableUrl":"https://www.bco-dmo.org/dataset/708293/data/view/901678","description":"Primary data file for dataset ID 708293","filename":"ctd_BH1511.csv","bytesize":576794,"checksum":{"value":"033b0f966d71ccc14d9a74cf7099f60b","Algorithm":{"_id":"190","name":"MD5"}},"mimetype":"text/csv","fileType":{"_id":"192","name":"Comma Separated Values (.csv)"},"isErddap":"bcodmo_dataset_708293","date":"","isPublicDuringEmbargo":false,"primaryDataFile":true,"showTable":true,"restricted":false}],"supplemental_files":[{"id":"774195","title":"BH15-11_CTD_Cast_sheets.pdf","url":"https://datadocs.bco-dmo.org/docs/horner/Great_Lakes_geochem/data_docs/BH15-11_CTD_Cast_sheets.pdf","showTableUrl":"","description":"BH15-11_CTD_Cast_sheets.pdf","filename":"BH15-11_CTD_Cast_sheets.pdf","bytesize":1564815,"checksum":{"value":"cd8dfd6fab1ec295514c222f9e9104e7","Algorithm":{"_id":"190","name":"MD5"}},"mimetype":"application/pdf","fileType":{"_id":"336","name":"Portable Document Format (.pdf)"},"isErddap":"","date":"","isPublicDuringEmbargo":false,"primaryDataFile":false,"showTable":false,"restricted":false}],"roles":[{"role":{"_id":"138","name":"Principal Investigator"},"performedBy":{"_id":"680928","name":"Tristan J. Horner"},"performedAtOrganization":{"_id":"2","name":"Woods Hole Oceanographic Institution"}},{"role":{"_id":"145","name":"BCO-DMO Data Manager"},"performedBy":{"_id":"51498","name":"Shannon Rauch"},"performedAtOrganization":{"_id":"191","name":"Woods Hole Oceanographic Institution"}}],"deployments":[{"_id":"685923","name":"BH15-11","synonyms":[],"dates":{"start":"2015-08-26T00:00:00.000Z","end":"2015-08-28T00:00:00.000Z"},"platform":{"_id":"54182","name":"R/V Blue Heron"},"chiefScientists":[]}],"funding":[{"_id":"679911","name":"OCE-1430015","fundingSource":{"_id":"355","name":"NSF Division of Ocean Sciences"},"url":"https://www.nsf.gov/awardsearch/show-award?AWD_ID=1430015"},{"_id":"680956","name":"OCE-1443577","fundingSource":{"_id":"355","name":"NSF Division of Ocean Sciences"},"url":"https://www.nsf.gov/awardsearch/show-award?AWD_ID=1443577"}],"instruments":[{"_id":"708836","name":"Sea-Bird SBE 9 and SBE 11plus V 5.0","description":"","type_id":"591","type_name":"CTD Sea-Bird SBE 911plus","type_desc":"The Sea-Bird SBE 911 plus is a type of CTD instrument package for continuous measurement of conductivity, temperature and pressure. The SBE 911 plus includes the SBE 9plus Underwater Unit and the SBE 11plus Deck Unit (for real-time readout using conductive wire) for deployment from a vessel. The combination of the SBE 9 plus and SBE 11 plus is called a SBE 911 plus. The SBE 9 plus uses Sea-Bird's standard modular temperature and conductivity sensors (SBE 3 plus and SBE 4). The SBE 9 plus CTD can be configured with up to eight auxiliary sensors to measure other parameters including dissolved oxygen, pH, turbidity, fluorescence, light (PAR), light transmission, etc.). more information from Sea-Bird Electronics","type_acronym":"CTD SBE 911plus"},{"_id":"708839","name":"WET Labs CDOM","description":"","type_id":"580","type_name":"CTD-fluorometer","type_desc":"A CTD-fluorometer is an instrument package designed to measure hydrographic information (pressure, temperature and conductivity) and chlorophyll fluorescence.","type_acronym":"CTD-fluorometer"},{"_id":"708842","name":"Biospherical/Licor","description":"","type_id":"480","type_name":"LI-COR Biospherical PAR Sensor","type_desc":"The LI-COR Biospherical PAR Sensor is used to measure Photosynthetically Available Radiation (PAR) in the water column. This instrument designation is used when specific make and model are not known.","type_acronym":"LI-COR Biospherical PAR"},{"_id":"708838","name":"SBE 43","description":"","type_id":"552","type_name":"Sea-Bird SBE 43 Dissolved Oxygen Sensor","type_desc":"The Sea-Bird SBE 43 dissolved oxygen sensor is a redesign of the Clark polarographic membrane type of dissolved oxygen sensors. More information from the manufacturer: https://www.seabird.com/products/sbe-43-dissolved-oxygen-sensor","type_acronym":"SBE-43 DO"},{"_id":"708837","name":"WET Labs WETstar","description":"","type_id":"474261","type_name":"WET Labs (Sea-Bird WETLabs) WETStar fluorometer","type_desc":"Submersible fluorometer designed for through-flow or pumped CTD applications manufactured by WetLabs and which can be configured for various types of fluorescence. The probe has a temperature range of 0-30 degrees C and a depth rating of 600 meters.","type_acronym":"WETStar"},{"_id":"708841","name":"WET Labs C-Star","description":"","type_id":"593","type_name":"WET Labs {Sea-Bird WETLabs} C-Star transmissometer","type_desc":"The C-Star transmissometer has a novel monolithic housing with a highly integrated opto-electronic design to provide a low cost, compact solution for underwater measurements of beam transmittance. The C-Star is capable of free space measurements or flow-through sampling when used with a pump and optical flow tubes. The sensor can be used in profiling, moored, or underway applications. Available with a 6000 m depth rating.\r\n\r\nMore information on Sea-Bird website: https://www.seabird.com/c-star-transmissometer/product?id=60762467717","type_acronym":"WL CSTAR Trans"}],"parameters":[{"_id":"708778","name":"cast","format":"","frictionlessType":"","description":"

Cast identier. Composed of station + cast (e.g. 002.01 = station 2, cast 1).

","units":{"_id":"","name":"unitless"},"type":{"_id":"761","name":"cast","description":"

cast or profile number

"}},{"_id":"708779","name":"lat_start","format":"","frictionlessType":"","description":"

Latitude at start of cast; obtained from .hdr files

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"870","name":"lat_start","description":"

latitude at start time of measurement; in decimal degrees (negative denotes South)

"}},{"_id":"708780","name":"lon_start","format":"","frictionlessType":"","description":"

Longitude at start of cast; obtained from .hdr files

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"883","name":"lon_start","description":"

longitude at starting time of measurement (west is negative), in decimal degrees

"}},{"_id":"708781","name":"ISO_DateTime_UTC","format":"","frictionlessType":"","description":"

Time and date formatted to ISO 8601 standard (yyyy-mm-ddTHH:MM:SS); obtained from .hdr files

","units":{"_id":"","name":"unitless"},"type":{"_id":"1908","name":"ISO_DateTime_UTC","description":"

Date/Time (UTC) ISO formatted
\nThis standard is based on ISO 8601:2004(E) and takes on any of the following forms:
\n2009-08-30T09:05:00[.xx] (local time)
\n2009-08-30T14:05:00[.xx]Z (UTC time)
\n2009-08-30T14:05:00[.xx]-05:00
\nThe dashes and the colons can be dropped.
\nThe T can also be dropped \"by mutual agreement\", but one needs the trailing Z if the time is UTC.

Sample ISO_datetime_utc:
\n2009-08-30T14:05:00[.xx]Z (UTC time)

Format: YYYY-mm-ddTHH:MM:SS[.xx]Z (UTC time)

"}},{"_id":"708782","name":"PrDM","format":"","frictionlessType":"","description":"

Pressure, Digiquartz

","units":{"_id":"","name":"decibars (db)"},"type":{"_id":"732","name":"pressure","description":"

water pressure at measurement; depth reported as pressure; positive number increasing with water depth

"}},{"_id":"708783","name":"DepFM","format":"","frictionlessType":"","description":"

Depth (fresh water)

","units":{"_id":"","name":"meters (m)"},"type":{"_id":"808","name":"depth","description":"

Observation/sample depth below the sea surface. Units often reported as: meters, feet.

\nWhen used in a JGOFS/GLOBEC dataset the depth is a best estimate; usually but not always calculated from pressure; calculated either from CTD pressure using Fofonoff and Millard (1982; UNESCO Tech Paper #44) algorithm adjusted for 1980 equation of state for seawater (EOS80) or simply equivalent to nominal depth as recorded during sampling if CTD pressure was unavailable.

"}},{"_id":"708784","name":"T090C","format":"","frictionlessType":"","description":"

Temperature [ITS-90]

","units":{"_id":"","name":"degrees Celsius"},"type":{"_id":"733","name":"temperature","description":"

water temperature at measurement depth

"}},{"_id":"708785","name":"C0uS_cm","format":"","frictionlessType":"","description":"

Conductivity

","units":{"_id":"","name":"microsiemens per centimeter (uS/cm)"},"type":{"_id":"779","name":"conductivity","description":"

Conductivity. Units and collection methods may vary. Often reported in Siemens/meter.

When used in a JGOFS/GLOBEC project this is the conductivity in Siemens/meter for the primary conductivity sensor on a CTD.

"}},{"_id":"708786","name":"Specc","format":"","frictionlessType":"","description":"

Specific conductance

","units":{"_id":"","name":"microsiemens per centimeter (uS/cm)"},"type":{"_id":"1894","name":"specific conductance","description":"

Electrical conductivity is a measure of a water’s ability to conduct electricity, and therefore a measure of the water’s ionic activity and content. The higher the concentration of ionic (dissolved) constituents, the higher the conductivity. Conductivity of the same water changes substantially as its temperature changes. This can have a confounding effect on attempts to compare this feature across different waters, or seasonal changes in this parameter for a particular body of water. The use of specific conductance [SC; units of microSiemens per centimeter (µS·cm-1) or miliSiemens per centimeter (mS·cm-1], the conductivity normalized to temperature of 25 ºC, eliminates this complication and allows valuable comparisons to be made.

"}},{"_id":"708787","name":"WetStar","format":"","frictionlessType":"","description":"

Fluorescence measured by WET Labs WETstar

","units":{"_id":"","name":"milligrams per cubic meter (mg/m3)"},"type":{"_id":"835","name":"fluorescence","description":"

Fluorescence. Indirect measure of pigment concentration.

Units and collection method may vary. Units often reported in milligrams/meter^3 (mg/m3) or micromoles per liter (ug/L). Sometimes reported after being calibrated against extracted pigment concentrations.

In JGOFS/GLOBEC projects fluorescence is measured from CTD instrument sensor.

"}},{"_id":"708788","name":"Sbeox0Mg_L","format":"","frictionlessType":"","description":"

Oxygen measured by SBE43

","units":{"_id":"","name":"milligrams per liter (mg/L)"},"type":{"_id":"910","name":"dissolved Oxygen","description":"

dissolved oxygen concentration

"}},{"_id":"708789","name":"WetCDOM","format":"","frictionlessType":"","description":"

Fluorescence measured by WET Labs CDOM

","units":{"_id":"","name":"milligrams per cubic meter (mg/m3)"},"type":{"_id":"835","name":"fluorescence","description":"

Fluorescence. Indirect measure of pigment concentration.

In JGOFS/GLOBEC projects fluorescence is measured from CTD instrument sensor.

"}},{"_id":"708790","name":"CStarTr0","format":"","frictionlessType":"","description":"

Beam transmission measured by WET Labs C-Star

","units":{"_id":"","name":"percent (%)"},"type":{"_id":"1013","name":"transmission","description":"

light transmission, as percent

"}},{"_id":"708791","name":"Par","format":"","frictionlessType":"","description":"

PAR/Irradiance measured by Biospherical/Licor

","units":{"_id":"","name":"microEinsteins per square centimeter per second (ueinsteins/cm2-sec)"},"type":{"_id":"913","name":"PAR","description":"

Photosynthetically Available [Active] Radiation; downwelling irradiance; units vary: often microEinsteins/meter^2/second, microEinsteins/centimeter^2/second, or micromoles photons/meter/second

"}},{"_id":"708792","name":"Orp","format":"","frictionlessType":"","description":"

Oxidation reduction potential

","units":{"_id":"","name":"millivolts (mV)"},"type":{"_id":"1073","name":"no_bcodmo_term","description":"

An association with a community-wide standard parameter has not yet been made.

"}},{"_id":"708793","name":"Ph","format":"","frictionlessType":"","description":"

","units":{"_id":"","name":"unitless (pH scale)"},"type":{"_id":"1892","name":"pH","description":"

pH: The measure of the acidity or basicity of an aqueous solution

"}},{"_id":"708794","name":"Dz_dtM","format":"","frictionlessType":"","description":"

Descent rate

","units":{"_id":"","name":"meters per second (m/s)"},"type":{"_id":"1893","name":"descent_rate","description":"

Descent rate of an instrument package

"}},{"_id":"708795","name":"TimeS","format":"","frictionlessType":"","description":"

Elapsed time

","units":{"_id":"","name":"seconds"},"type":{"_id":"1838","name":"time_elapsed","description":"

Elapsed time. Units can be seconds, minutes, etc.

"}},{"_id":"708796","name":"AltM","format":"","frictionlessType":"","description":"

Altimeter

","units":{"_id":"","name":"meter (m)"},"type":{"_id":"1839","name":"altitude","description":"

Altitude of sampler above the bottom

"}},{"_id":"708797","name":"Latitude","format":"","frictionlessType":"","description":"

Latitude

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"730","name":"latitude","description":"

latitude, in decimal degrees, North is positive, negative denotes South; Reported in some datasets as degrees, minutes

"}},{"_id":"708798","name":"Longitude","format":"","frictionlessType":"","description":"

Longitude

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"731","name":"longitude","description":"

longitude, in decimal degrees, East is positive, negative denotes West; Reported in some datasets as degrees, minutes

"}},{"_id":"708799","name":"Nbin","format":"","frictionlessType":"","description":"

Number of scans per bin

","units":{"_id":"","name":"unitless"},"type":{"_id":"899","name":"nbin","description":"

reported with CTD data, refers to the number of data cycles used to compile an average value for a given depth/BIN interval.

"}},{"_id":"708800","name":"Flag","format":"","frictionlessType":"","description":"

0.000e+00 (bad flag = -9.990e-29)

","units":{"_id":"","name":"unitless"},"type":{"_id":"1730","name":"flag","description":"

Data flag. Multiple uses which are dataset dependent. Some uses: data quality, collection occurrence or success, depth indicator. See dataset documentation for specific details

"}},{"_id":"709400","name":"station_name","format":"","frictionlessType":"","description":"

Name commonly used to refer to the station

","units":{"_id":"","name":"unitless"},"type":{"_id":"1104","name":"sta_name","description":"

station name; a unique combination of alpha and/or numeric characters designating a general geographic location at which one or more sampling activities may occur.

"}}],"related_publications":[{"id":"774194","citation":"Horner, T. J., Pryer, H. V., Nielsen, S. G., Crockford, P. W., Gauglitz, J. M., Wing, B. A., & Ricketts, R. D. (2017). Pelagic barite precipitation at micromolar ambient sulfate. Nature Communications, 8(1). doi:10.1038/s41467-017-01229-5\r\n","relation_type":["Results"],"relation_desc":""}],"related_datasets":[],"services":[{"grouping":"","items":[{"name":"View Data","description":"An in-browser view of the primary tabular data file","url":"https://www.bco-dmo.org/dataset/708293/data/view","contentType":"text/html","actionType":"view"}]},{"grouping":"ERDDAP","items":[{"name":"SUBSET DATA","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.html","contentType":"text/html","actionType":"tool"},{"name":"VIEW TABLE","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.htmlTable","contentType":"text/html","actionType":"view"},{"name":"CSV","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.csv","contentType":"text/csv","actionType":"download"},{"name":"TSV","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.tsv","contentType":"text/tsv","actionType":"download"},{"name":"GeoJSON","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.geoJson","contentType":"application/geo+json","actionType":"download"},{"name":"MATLAB","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.mat","contentType":"text/x-matlab","actionType":"download"},{"name":"netCDF","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.nc","contentType":"application/x-netcdf","actionType":"download"},{"name":"ODV","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_708293.odvTxt","contentType":"text/plain","actionType":"download"}]},{"grouping":"Metadata","items":[{"name":"HTML","description":"A simple HTML page of the dataset metadata","url":"https://www.bco-dmo.org/dataset/708293/description","contentType":"text/html","actionType":"view"},{"name":"PDF","description":"A PDF of the HTML dataset metadata","url":"https://www.bco-dmo.org/dataset/708293/Dataset_description.pdf","contentType":"application/pdf","actionType":"download"},{"name":"ISO 19115-2 (NOAA Profile)","description":"","url":"https://www.bco-dmo.org/dataset/708293/iso","contentType":"application/xml","actionType":"download"}]}],"programs":[],"projects":[{"_id":"679912","name":"EAGER - Introducing Early Career Scientists to Research on the Great Lakes","acronym":"Early Career Great Lakes research","description":"$1b"},{"_id":"680957","name":"Calibration of a Novel Nutrient Paleoproxy in the Southern Ocean","acronym":"Novel Nutrient Paleoproxy","description":"$1c"}],"archives":[{"id_value":"10.1575/1912/bco-dmo.708293.1","url":"https://doi.org/10.1575/1912/bco-dmo.708293.1","date_assigned":"2019-08-02","version_date":"2017-07-20","archiver":"Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)","archiver_id":"272"}],"license":{"name":"Creative Commons Attribution 4.0","id":"CC-BY-4.0","uri":"https://creativecommons.org/licenses/by/4.0/","spdxUri":"https://spdx.org/licenses/CC-BY-4.0"},"metrics":{"views":{"count":196},"downloads":{"count":527}}}}]