BCO-DMO ERDDAP
Accessing BCO-DMO data 		log in    
Brought to you by BCO-DMO    
 
 
Row Type Variable Name Attribute Name Data Type Value
attribute NC_GLOBAL access_formats String .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson,.odvTxt
attribute NC_GLOBAL acquisition_description String Sediment and pore water collection:\n \nShort sediment cores were collected using a Bowers & Connelly megacorer, a\nmultiple coring device that can collect ~20-40 cm long sediment cores with\nundisturbed sediment surfaces. At two sites (stations 41 and 64) longer cores\n(up to ~2 m) were also collected with a Kasten corer.\n \nMegacorer cores were either sectioned for solid phase analysis, profiled with\npolarographic microelectrodes to determine dissolved O2 concentrations, or\nsectioned in a cold van under N2 for pore water sample extraction (for details\nsee, Komada et al., 2016). Kasten cores were brought into a large cold room\non-board ship, laid on their side and one side of the core box removed to\nexpose the sediment in the core. A plastic block was placed against the top of\nthe core to prevent slumping of the sediment during processing, and pore\nwaters were collected from these cores using Rhizon samplers (Seeberg-\nElverfeldt et al., 2005) inserted directly into the cores at measured\nintervals.\n \nPore water samples collected from both types of cores were filtered through\n0.45 \\u00b5m polycarbonate filters and processed as follows. Samples for\nalkalinity determinations were stored without a headspace in 3-ml plastic\nsyringes sealed with 3-way stopcocks. Titrated alkalinity samples (acidified\nto pH ~4 after titration) were stored in plastic snap cap vials, refrigerated\nand returned to ODU for the analysis of dissolved sulfate. Pore water samples\ncollected for the analysis of total dissolved Fe and Mn were acidified to pH\n<2 on-board ship with trace metal grade HCl, and store refrigerated until\nanalyzed back at ODU. Samples for pore water silicate analyses were analyzed\non board the research vessel. Additional samples for the analysis of other\ndissolved nutrients (nitrate, nitrite, ammonium, phosphate) were filtered into\ntightly capped sample vials and frozen for return to NEOL for analysis.\nSelected pore water samples (collected as described above) were also used for\nthe determination of dissolved organic carbon (DOC). These samples were\nfiltered directly into acid-cleaned and muffled (550 \\u00b0C for at least 4 h)\nglass ampules and were then acidified to pH < 2 with 6 N trace metal grade HCl\nand flame-sealed under a stream of UHP N2 gas. The sealed ampules were stored\nrefrigerated and returned to ODU for analysis.\n \nWhile it is possible to recover cores with intact sediment-water interfaces\nusing a megacorer, loss of surface sediments is typical during Kasten coring,\nmaking it not possible to directly determine absolute depths below the\nsediment-water interface in a Kasten core. We therefore determined the\nabsolute depths of pore water and solid phase sample intervals from Kasten\ncores by aligning Kasten core profiles of pore water alkalinity to megacore\nalkalinity profiles from the same site (Berelson et al., 2005; Komada et al.,\n2016).\n \nBottom water collection:\n \nBottom waters were collected by GO-Flo Bottles ~5-10 m off the seafloor. They\nwere filtered through 0.45 \\u00b5m polycarbonate filters and processed as\ndescribed above for pore water samples.\n \nPore water analyses: Sampled collected for alkalinity determination were\ntitrated aboard ship within 12 hours of collection by automated Gran titration\n(Hu and Burdige, 2008). Dissolved sulfate was determined on titrated\nalkalinity samples returned to ODU by ion chromatography and conductivity\ndetection (Thermo-Scientific Dionex ICS-5000; Burdige and Komada, 2011; Komada\net al., 2016). Concentrations of DOC were determined at ODU by high\ntemperature combustion using a Shimadzu TOC-V total carbon analyzer (Komada et\nal., 2013; Komada et al., 2016). Frozen samples for the determination of\ndissolved nutrients were returned to NEOL and analyzed by autoanalyzer for\nnitrate and nitrite (Armstrong et al., 1967; Pavlou, 1972), ammonium\n(Koroleff, 1970; Slawyk and MacIsaac, 1972) and dissolved inorganic phosphate\n(Drummond and Maher, 1995). Pore water silicate was determined on board the\nresearch vessel used fresh pore water samples and a manual colorimetric method\nfollowing Armstrong et al. (1967).\n \nPore water dissolved iron was determined colorimetrically at ODU using the\nferrozine technique (Stookey, 1970; Viollier et al., 2000). Hydroxylamine-HCl\n(0.2% final concentration) was added to the samples before analysis, to reduce\nany dissolved Fe3+ in the samples to Fe2+. The pore water iron results\nreported here therefore represent total dissolved iron (i.e., Fe2+ plus any\nFe3+ in the samples). This was done largely as a precaution against any iron\noxidation that may have occurred during sample storage, since it is assumed\nthat virtually all of the dissolved iron in these pore waters exists in situ\nas Fe2+ (e.g., Viollier et al., 2000).\n \nSamples for the analysis of dissolved manganese were determined with a\nmodification of the colorimetric formaldoxime method (Armstrong et al., 1979;\nGoto et al., 1962). These modifications were made based on the observation\nthat the amount of EDTA typically added to destroy the Fe-formaldoxime\ncomplexes that interfere with the colorimetric determination of the Mn-\nformaldoxime complexes was insufficient because of the complexation (and\npresumed competition) of this EDTA by the much higher levels of dissolved Ca2+\nand Mg2+ in our pore water samples ( 60 mM assuming a pore water salinity of\n~35). Thus it was necessary to increase the amount of EDTA added to the\nsamples so that it exceeded these Ca2+ plus Mg2+ levels.\n \nIn our method we made the formaldoxime mixed reagent by dissolving 8 g of\nhydroxylamine hydrochloride and 4ml formaldehyde (37%) in 200 ml of distilled\ndeionized water. Next we combined 0.5 ml of either a pore water sample or Mn2+\nstandard with 0.5 ml of distilled deionized water and: 50 \\u00b5l of the\nformaldoxime mixed reagent, 50 \\u00b5l of concentrated (50%) NH4OH, 50 \\u00b5l\nof a 20% hydroxylamine hydrochloride solution, and 0.2 ml of a 250 mM EDTA\nsolution. The color of the solution was allowed to develop for 20 min. and\nthen analyzed at 450 nm.
attribute NC_GLOBAL awards_0_award_nid String 806863
attribute NC_GLOBAL awards_0_award_number String OPP-1551195
attribute NC_GLOBAL awards_0_data_url String http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1551195 (external link)
attribute NC_GLOBAL awards_0_funder_name String NSF Division of Ocean Sciences
attribute NC_GLOBAL awards_0_funding_acronym String NSF OCE
attribute NC_GLOBAL awards_0_funding_source_nid String 355
attribute NC_GLOBAL awards_0_program_manager String Michael E. Jackson
attribute NC_GLOBAL awards_0_program_manager_nid String 806862
attribute NC_GLOBAL cdm_data_type String Other
attribute NC_GLOBAL comment String Pore water geochemistry \n  PI: David J Burdige \n  Data Version 1: 2020-06-08
attribute NC_GLOBAL Conventions String COARDS, CF-1.6, ACDD-1.3
attribute NC_GLOBAL creator_email String info at bco-dmo.org
attribute NC_GLOBAL creator_name String BCO-DMO
attribute NC_GLOBAL creator_type String institution
attribute NC_GLOBAL creator_url String https://www.bco-dmo.org/ (external link)
attribute NC_GLOBAL data_source String extract_data_as_tsv version 2.3  19 Dec 2019
attribute NC_GLOBAL dataset_current_state String Final and no updates
attribute NC_GLOBAL date_created String 2020-05-27T22:59:42Z
attribute NC_GLOBAL date_modified String 2020-06-17T23:05:28Z
attribute NC_GLOBAL defaultDataQuery String &amp;time&lt;now
attribute NC_GLOBAL doi String 10.26008/1912/bco-dmo.813166.1
attribute NC_GLOBAL Easternmost_Easting double -62.7317
attribute NC_GLOBAL geospatial_lat_max double -64.1583
attribute NC_GLOBAL geospatial_lat_min double -67.7717
attribute NC_GLOBAL geospatial_lat_units String degrees_north
attribute NC_GLOBAL geospatial_lon_max double -62.7317
attribute NC_GLOBAL geospatial_lon_min double -71.2217
attribute NC_GLOBAL geospatial_lon_units String degrees_east
attribute NC_GLOBAL infoUrl String https://www.bco-dmo.org/dataset/813166 (external link)
attribute NC_GLOBAL institution String BCO-DMO
attribute NC_GLOBAL instruments_0_acronym String GO-FLO
attribute NC_GLOBAL instruments_0_dataset_instrument_nid String 814590
attribute NC_GLOBAL instruments_0_description String GO-FLO bottle cast used to collect water samples for pigment, nutrient, plankton, etc. The GO-FLO sampling bottle is specially designed to avoid sample contamination at the surface, internal spring contamination, loss of sample on deck (internal seals), and exchange of water from different depths.
attribute NC_GLOBAL instruments_0_instrument_external_identifier String https://vocab.nerc.ac.uk/collection/L05/current/30/ (external link)
attribute NC_GLOBAL instruments_0_instrument_name String GO-FLO Bottle
attribute NC_GLOBAL instruments_0_instrument_nid String 411
attribute NC_GLOBAL instruments_1_acronym String Gravity Corer
attribute NC_GLOBAL instruments_1_dataset_instrument_nid String 814589
attribute NC_GLOBAL instruments_1_description String The gravity corer allows researchers to sample sediment layers at the bottom of lakes or oceans. The coring device is deployed from the ship and gravity carries it to the seafloor. (https://www.whoi.edu/instruments/viewInstrument.do?id=1079).
attribute NC_GLOBAL instruments_1_instrument_external_identifier String https://vocab.nerc.ac.uk/collection/L05/current/51/ (external link)
attribute NC_GLOBAL instruments_1_instrument_name String Gravity Corer
attribute NC_GLOBAL instruments_1_instrument_nid String 531
attribute NC_GLOBAL instruments_1_supplied_name String Kasten corer
attribute NC_GLOBAL instruments_2_acronym String Multi Corer
attribute NC_GLOBAL instruments_2_dataset_instrument_nid String 814588
attribute NC_GLOBAL instruments_2_description String The Multi Corer is a benthic coring device used to collect multiple, simultaneous, undisturbed sediment/water samples from the seafloor.  Multiple coring tubes with varying sampling capacity depending on tube dimensions are mounted in a frame designed to sample the deep ocean seafloor. For more information, see Barnett et al. (1984) in Oceanologica Acta, 7, pp. 399-408.
attribute NC_GLOBAL instruments_2_instrument_external_identifier String https://vocab.nerc.ac.uk/collection/L05/current/51/ (external link)
attribute NC_GLOBAL instruments_2_instrument_name String Multi Corer
attribute NC_GLOBAL instruments_2_instrument_nid String 532
attribute NC_GLOBAL instruments_2_supplied_name String Bowers & Connelly megacorer
attribute NC_GLOBAL instruments_3_acronym String Nutrient Autoanalyzer
attribute NC_GLOBAL instruments_3_dataset_instrument_description String Frozen samples for the determination of dissolved nutrients were returned to NEOL and analyzed by autoanalyzer for nitrate and nitrite (Armstrong et al., 1967; Pavlou, 1972), ammonium (Koroleff, 1970; Slawyk and MacIsaac, 1972) and dissolved inorganic phosphate (Drummond and Maher, 1995).
attribute NC_GLOBAL instruments_3_dataset_instrument_nid String 814592
attribute NC_GLOBAL instruments_3_description String Nutrient Autoanalyzer is a generic term used when specific type, make and model were not specified.  In general, a Nutrient Autoanalyzer is an automated flow-thru system for doing nutrient analysis (nitrate, ammonium, orthophosphate, and silicate) on seawater samples.
attribute NC_GLOBAL instruments_3_instrument_external_identifier String https://vocab.nerc.ac.uk/collection/L05/current/LAB04/ (external link)
attribute NC_GLOBAL instruments_3_instrument_name String Nutrient Autoanalyzer
attribute NC_GLOBAL instruments_3_instrument_nid String 558
attribute NC_GLOBAL instruments_4_acronym String Shimadzu TOC-V
attribute NC_GLOBAL instruments_4_dataset_instrument_nid String 814591
attribute NC_GLOBAL instruments_4_description String A Shimadzu TOC-V Analyzer measures DOC by high temperature combustion method.
attribute NC_GLOBAL instruments_4_instrument_external_identifier String http://onto.nerc.ac.uk/CAST/124 (external link)
attribute NC_GLOBAL instruments_4_instrument_name String Shimadzu TOC-V Analyzer
attribute NC_GLOBAL instruments_4_instrument_nid String 603
attribute NC_GLOBAL instruments_4_supplied_name String Shimadzu TOC-V total carbon analyzer (Komada et al., 2013; Komada et al., 2016).
attribute NC_GLOBAL keywords String alk, ammonia, ammonium, bco, bco-dmo, biological, chemical, chemistry, commerce, concentration, core, data, dataset, date, department, depth, dmo, doc, earth, Earth Science > Oceans > Ocean Chemistry > Ammonia, Earth Science > Oceans > Ocean Chemistry > Nitrate, Earth Science > Oceans > Ocean Chemistry > pH, Earth Science > Oceans > Ocean Chemistry > Phosphate, Earth Science > Oceans > Ocean Chemistry > Silicate, erddap, error, iso, latitude, longitude, management, mass, mass_concentration_of_phosphate_in_sea_water, mass_concentration_of_silicate_in_sea_water, mole, mole_concentration_of_ammonium_in_sea_water, mole_concentration_of_nitrate_in_sea_water, mole_concentration_of_nitrite_in_sea_water, n02, nh4, nitrate, nitrite, NO2, no3, ocean, oceanography, oceans, office, phosphate, po4, preliminary, reported, Sa_ID, samp, scale, science, sea, sea_water_ph_reported_on_total_scale, seawater, silicate, so4, St_ID, time, total, water
attribute NC_GLOBAL keywords_vocabulary String GCMD Science Keywords
attribute NC_GLOBAL license String https://www.bco-dmo.org/dataset/813166/license (external link)
attribute NC_GLOBAL metadata_source String https://www.bco-dmo.org/api/dataset/813166 (external link)
attribute NC_GLOBAL Northernmost_Northing double -64.1583
attribute NC_GLOBAL param_mapping String {'813166': {'Lat': 'master - latitude', 'Lon': 'master - longitude', 'ISO_DateTime_UTC': 'master - time'}}
attribute NC_GLOBAL parameter_source String https://www.bco-dmo.org/mapserver/dataset/813166/parameters (external link)
attribute NC_GLOBAL people_0_affiliation String Old Dominion University
attribute NC_GLOBAL people_0_affiliation_acronym String ODU
attribute NC_GLOBAL people_0_person_name String David J Burdige
attribute NC_GLOBAL people_0_person_nid String 648653
attribute NC_GLOBAL people_0_role String Principal Investigator
attribute NC_GLOBAL people_0_role_type String originator
attribute NC_GLOBAL people_1_affiliation String New England Oceanographic Laboratory
attribute NC_GLOBAL people_1_affiliation_acronym String NEOL
attribute NC_GLOBAL people_1_person_name String John P Christensen
attribute NC_GLOBAL people_1_person_nid String 51603
attribute NC_GLOBAL people_1_role String Co-Principal Investigator
attribute NC_GLOBAL people_1_role_type String originator
attribute NC_GLOBAL people_2_affiliation String Woods Hole Oceanographic Institution
attribute NC_GLOBAL people_2_affiliation_acronym String WHOI BCO-DMO
attribute NC_GLOBAL people_2_person_name String Amber D. York
attribute NC_GLOBAL people_2_person_nid String 643627
attribute NC_GLOBAL people_2_role String BCO-DMO Data Manager
attribute NC_GLOBAL people_2_role_type String related
attribute NC_GLOBAL project String Antarctic Shelf Sediments
attribute NC_GLOBAL projects_0_acronym String Antarctic Shelf Sediments
attribute NC_GLOBAL projects_0_description String NSF Award Abstract:\nGeneral Statement:\nThe continental shelf region west of the Antarctic Peninsula has recently undergone dramatic changes and ecosystem shifts, and the community of organisms that live in, or feed off, the sea floor sediments is being impacted by species invasions from the north. Previous studies of these sediments indicate that this community may consume much more of the regional productivity than previously estimated, suggesting that sediments are a rich and important component of this ecosystem and one that may be ripe for dramatic change. Furthermore, under richer sediment conditions, iron is mobilized and released back to the water column. Since productivity in this ecosystem is thought to be limited by the availability of iron, increased rates of iron release from these sediments could stimulate productivity and promote greater overall ecosystem change. In this research, a variety of sites across the shelf region will be sampled to accurately evaluate the role of sediments in consuming ecosystem productivity and to estimate the current level of iron release from the sediments. This project will provide a baseline set of sediment results that will present a more complete picture of the west Antarctic shelf ecosystem, will allow for comparison with water column measurements and for evaluation of the fundamental workings of this important ecosystem. This is particularly important since high latitude systems may be vulnerable to the effects of climate fluctuations. Both graduate and undergraduate students will be trained. Presentations will be made at scientific meetings, at other universities, and at outreach events. A project web site will present key results to the public and explain how this new information improves understanding of Antarctic ecosystems.\n\nTechnical Description of Project:\nIn order to determine the role of sediments within the west Antarctic shelf ecosystem, this project will determine the rates of sediment organic matter oxidation at a variety of sites across the Palmer Long Term Ecosystem Research (LTER) study region. To estimate the rates of release of iron and manganese from the sediments, these same sites will be sampled for detailed vertical distributions of the concentrations of these metals both in the porewaters and in important mineral phases. Since sediment sampling will be done at LTER sites, the sediment data can be correlated with the rich productivity data set from the LTER. In detail, the project: a) will determine the rates of oxygen consumption, organic carbon oxidation, nutrient release, and iron mobilization by shelf sediments west of the Antarctic Peninsula; b) will investigate the vertical distribution of diagenetic reactions within the sediments; and c) will assess the regional importance of these sediment rates. Sediment cores will be used to determine sediment-water fluxes of dissolved oxygen, total carbon dioxide, nutrients, and the vertical distributions of these dissolved compounds, as well as iron and manganese in the pore waters. Bulk sediment properties of porosity, organic carbon and nitrogen content, carbonate content, biogenic silica content, and multiple species of solid-phase iron, manganese, and sulfur species will also be determined. These measurements will allow determination of total organic carbon oxidation and denitrification rates, and the proportion of aerobic versus anaerobic respiration at each site. Sediment diagenetic modeling will link the processes of organic matter oxidation to metal mobilization. Pore water and solid phase iron and manganese distributions will be used to model iron diagenesis in these sediments and to estimate the iron flux from the sediments to the overlying waters. Finally, the overall regional average and distribution of the sediment processes will be compared with the distributions of seasonally averaged chlorophyll biomass and productivity.
attribute NC_GLOBAL projects_0_end_date String 2020-02
attribute NC_GLOBAL projects_0_geolocation String West Antarctic Continental Shelf
attribute NC_GLOBAL projects_0_name String Organic Carbon Oxidation and Iron Remobilization by West Antarctic Shelf Sediments
attribute NC_GLOBAL projects_0_project_nid String 806864
attribute NC_GLOBAL projects_0_start_date String 2015-09
attribute NC_GLOBAL publisher_name String Biological and Chemical Oceanographic Data Management Office (BCO-DMO)
attribute NC_GLOBAL publisher_type String institution
attribute NC_GLOBAL sourceUrl String (local files)
attribute NC_GLOBAL Southernmost_Northing double -67.7717
attribute NC_GLOBAL standard_name_vocabulary String CF Standard Name Table v55
attribute NC_GLOBAL summary String Pore water geochemistry from sediment cores collected on the R/V Nathaniel B. Palmer cruise NBP1601 to the West Antarctic continental shelf in January of 2016.
attribute NC_GLOBAL time_coverage_end String 2019-01-28T09:36Z
attribute NC_GLOBAL time_coverage_start String 2016-01-14T17:34Z
attribute NC_GLOBAL title String [Pore water geochemistry] - Pore water geochemistry from sediment cores collected on the R/V Nathaniel B. Palmer cruise NBP1601 to the West Antarctic continental shelf in January of 2016 (Organic Carbon Oxidation and Iron Remobilization by West Antarctic Shelf Sediments)
attribute NC_GLOBAL version String 1
attribute NC_GLOBAL Westernmost_Easting double -71.2217
attribute NC_GLOBAL xml_source String osprey2erddap.update_xml() v1.5
variable St_ID String
attribute St_ID bcodmo_name String station
attribute St_ID description String station ID #
attribute St_ID long_name String St ID
attribute St_ID units String unitless
variable Sa_ID String
attribute Sa_ID bcodmo_name String sample
attribute Sa_ID description String sample ID (station ID #- core ID #-sample # (BW = bottom water sample; note BW samples have no sample #)
attribute Sa_ID long_name String Sa ID
attribute Sa_ID nerc_identifier String https://vocab.nerc.ac.uk/collection/P02/current/ACYC/ (external link)
attribute Sa_ID units String unitless
variable Core String
attribute Core bcodmo_name String sample_type
attribute Core description String core type (H = samples collected by hydrocast; M = mega-corer; K = Kasten corer)
attribute Core long_name String Core
attribute Core units String unitless
variable Samp String
attribute Samp bcodmo_name String sample_descrip
attribute Samp description String how pore waters/bottom waters were collected (C = centrifugation; R = rhizon sampler; G = hydrocast/GO-Flo bottle; see Methodology for details)
attribute Samp long_name String Samp
attribute Samp units String unitless
variable Depth float
attribute Depth _FillValue float NaN
attribute Depth actual_range float 0.0, 225.0
attribute Depth bcodmo_name String depth_bsf
attribute Depth colorBarMaximum double 8000.0
attribute Depth colorBarMinimum double -8000.0
attribute Depth colorBarPalette String TopographyDepth
attribute Depth description String sediment depth (relative to the sediment-water interface; 0 = bottom water sample)
attribute Depth long_name String Depth
attribute Depth standard_name String depth
attribute Depth units String centimeters (cm)
variable Error float
attribute Error _FillValue float NaN
attribute Error actual_range float 0.25, 1.5
attribute Error bcodmo_name String sample_descrip
attribute Error colorBarMaximum double 50.0
attribute Error colorBarMinimum double 0.0
attribute Error description String half the thickness of the sediment sample (note: Rhizon samples are collected at discrete depths and there is no error associated with their depths)
attribute Error long_name String Error
attribute Error units String centimeters (cm)
variable pH float
attribute pH _FillValue float NaN
attribute pH actual_range float 0.0, 7.69
attribute pH bcodmo_name String pH
attribute pH colorBarMaximum double 9.0
attribute pH colorBarMinimum double 7.0
attribute pH description String initial pH of sample titrated for alkalinity
attribute pH long_name String Sea Water Ph Reported On Total Scale
attribute pH nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/PHXXZZXX/ (external link)
attribute pH units String NBS scale
variable Alk float
attribute Alk _FillValue float NaN
attribute Alk actual_range float 0.0, 6.95
attribute Alk bcodmo_name String TALK
attribute Alk description String pore water alkalinity
attribute Alk long_name String Alk
attribute Alk nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/MDMAP014/ (external link)
attribute Alk units String millimolar (mM)
variable Fe float
attribute Fe _FillValue float NaN
attribute Fe actual_range float 0.0, 85.84
attribute Fe bcodmo_name String Fe
attribute Fe description String pore water total dissolved iron
attribute Fe long_name String Fe
attribute Fe units String micromolar (uM)
variable Mn float
attribute Mn _FillValue float NaN
attribute Mn actual_range float 0.0, 16.23
attribute Mn bcodmo_name String Mn
attribute Mn description String pore water dissolved Mn
attribute Mn long_name String MN
attribute Mn units String micromolar (uM)
variable SO4 float
attribute SO4 _FillValue float NaN
attribute SO4 actual_range float 21.52, 34.0
attribute SO4 bcodmo_name String SO4
attribute SO4 description String pore water dissolved sulfate
attribute SO4 long_name String SO4
attribute SO4 nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/SPHTMAXX/ (external link)
attribute SO4 units String millimolar (mM)
variable DOC float
attribute DOC _FillValue float NaN
attribute DOC actual_range float 74.62, 1821.34
attribute DOC bcodmo_name String DOC
attribute DOC description String pore water dissolved organic carbon
attribute DOC long_name String DOC
attribute DOC nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/CORGZZZX/ (external link)
attribute DOC units String micromolar (uM)
variable NO3 float
attribute NO3 _FillValue float NaN
attribute NO3 actual_range float 0.0, 37.77
attribute NO3 bcodmo_name String NO3
attribute NO3 colorBarMaximum double 50.0
attribute NO3 colorBarMinimum double 0.0
attribute NO3 description String pore water dissolved nitrate
attribute NO3 long_name String Mole Concentration Of Nitrate In Sea Water
attribute NO3 nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/NTRAIGGS/ (external link)
attribute NO3 units String micromolar (uM)
variable NO2 float
attribute NO2 _FillValue float NaN
attribute NO2 actual_range float 0.0, 3.42
attribute NO2 bcodmo_name String NO2
attribute NO2 colorBarMaximum double 1.0
attribute NO2 colorBarMinimum double 0.0
attribute NO2 description String pore water dissolved nitrite
attribute NO2 long_name String Mole Concentration Of Nitrite In Sea Water
attribute NO2 nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/NTRIAAZX/ (external link)
attribute NO2 units String micromolar (uM)
variable NH4 float
attribute NH4 _FillValue float NaN
attribute NH4 actual_range float 0.0, 263.5
attribute NH4 bcodmo_name String Ammonium
attribute NH4 colorBarMaximum double 5.0
attribute NH4 colorBarMinimum double 0.0
attribute NH4 description String pore water dissolved ammonium
attribute NH4 long_name String Mole Concentration Of Ammonium In Sea Water
attribute NH4 nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/AMONAAZX/ (external link)
attribute NH4 units String micromolar (uM)
variable PO4 float
attribute PO4 _FillValue float NaN
attribute PO4 actual_range float 6.35, 41.6
attribute PO4 bcodmo_name String PO4
attribute PO4 description String pore water dissolved orthophosphate
attribute PO4 long_name String Mass Concentration Of Phosphate In Sea Water
attribute PO4 units String micromolar (uM)
variable Si float
attribute Si _FillValue float NaN
attribute Si actual_range float 155.1, 838.2
attribute Si bcodmo_name String Si
attribute Si description String pore water dissolved silicate
attribute Si long_name String Mass Concentration Of Silicate In Sea Water
attribute Si units String micromolar (uM)
variable time double
attribute time _CoordinateAxisType String Time
attribute time actual_range double 1.45279284E9, 1.54866816E9
attribute time axis String T
attribute time bcodmo_name String ISO_DateTime_UTC
attribute time description String station timestamp (UTC) in ISO 8601 format yyyy-mm-ddTHH:MMZ
attribute time ioos_category String Time
attribute time long_name String ISO Date Time UTC
attribute time nerc_identifier String https://vocab.nerc.ac.uk/collection/P01/current/DTUT8601/ (external link)
attribute time source_name String ISO_DateTime_UTC
attribute time standard_name String time
attribute time time_origin String 01-JAN-1970 00:00:00
attribute time time_precision String 1970-01-01T00:00Z
attribute time units String seconds since 1970-01-01T00:00:00Z
variable latitude double
attribute latitude _CoordinateAxisType String Lat
attribute latitude _FillValue double NaN
attribute latitude actual_range double -67.7717, -64.1583
attribute latitude axis String Y
attribute latitude bcodmo_name String latitude
attribute latitude colorBarMaximum double 90.0
attribute latitude colorBarMinimum double -90.0
attribute latitude description String station latitude, south is negative
attribute latitude ioos_category String Location
attribute latitude long_name String Latitude
attribute latitude nerc_identifier String https://vocab.nerc.ac.uk/collection/P09/current/LATX/ (external link)
attribute latitude standard_name String latitude
attribute latitude units String degrees_north
variable longitude double
attribute longitude _CoordinateAxisType String Lon
attribute longitude _FillValue double NaN
attribute longitude actual_range double -71.2217, -62.7317
attribute longitude axis String X
attribute longitude bcodmo_name String longitude
attribute longitude colorBarMaximum double 180.0
attribute longitude colorBarMinimum double -180.0
attribute longitude description String station longitude, west is negative
attribute longitude ioos_category String Location
attribute longitude long_name String Longitude
attribute longitude nerc_identifier String https://vocab.nerc.ac.uk/collection/P09/current/LONX/ (external link)
attribute longitude standard_name String longitude
attribute longitude units String degrees_east

 
ERDDAP, Version 2.22
Disclaimers | Privacy Policy | Contact