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Row Type | Variable Name | Attribute Name | Data Type | Value |
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attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson,.odvTxt |
attribute | NC_GLOBAL | acquisition_description | String | Methodology: \n Dissolved inorganic carbon concentration ([DIC]) samples were measured by\nacidification and subsequent release of CO2 with a CO2 cavity-ringdown\nspectrometer (CRDS; Picarro G1101-i) detector to an accuracy and precision\nbetter than \\u00b1 3 umol/kg. Precision is based on a set of 15 duplicates.\nAccuracy is based on certified reference materials prepared at the Scripps\nInstitution of Oceanography of the University of California, San Diego.\n \nSamples for pH were measured spectrophotometrically on board using an Agilent\nCary 100 UV-Visible spectrophotometer and m-cresol purple dye (Clayton and\nByrne, 1993; Liu et al., 2011). The pH values are reported on the total scale\nwith a precision better than 0.0002 based on duplicate measurements. The\nestimated accuracy of spectrophotometric pH is better than 0.002.\n \nNatural radiocarbon samples of DIC (\\u220614C-DIC) were analyzed at the W. M.\nKeck Carbon Cycle Accelerator Mass Spectrometry Laboratory at the University\nof California, Irvine. The accuracy and precision of the \\u220614C-DIC\nmeasurements is 0.1\\u2030 and 1.7\\u2030, respectively.\n \nSampling and analytical procedures:\\u00a0 \n Discrete seawater samples were collected inside Hudson Canyon, US Atlantic\nMargin aboard the R/V Endeavor from 9 - 13 of July 2014. A total 19 stations\nand 216 samples were collected along Hudson Canyon and another station was\nsampled outside the canyon (station E2-HC2). Samples were collected from a\nbottle Rosette following the procedures in SOP 1 and 6b in Dickson et al.,\n(2007).\n \n[DIC] samples were collected in acid washed and combusted 120 mL serum vials.\nVials were allowed to overflow three times their volume, poisoned with 50 uL\nof a 55 uM HgCl2, capped, and store at 4 degrees C\\u00a0until analysis.\n \n\\u220614C-DIC samples were collected in combusted 1L borosilicate bottles,\npoisoned with 200 uL of a 55 uM HgCl2, sealed and stored in the dark at room\ntemperature until isotope analysis.\n \nCH4 concentration analyses were collected by filling 60, 120, or 160 mL glass\nserum vials. Vials were filled from the bottom with a length of 1/4\\\" Tygon\ntubing. Vials were flushed with seven vial volumes of seawater to expel any\nbubbles and ensure collection of a clean sample, and then were sealed with\nbutyl rubber stoppers taking care not to introduce bubbles during sealing.\nImmediately after sealing, a 10 mL headspace of ultrahigh purity nitrogen was\nintroduced, displacing an equal volume of water, and the samples were\npreserved by adding 25 uL of a saturated solution of mercuric chloride. The\nvials were stored inverted to minimize diffusive gas exchange through the\nbutyl rubber stopper.\n \nCH4 concentration measurements were performed using an Agilent 6850 gas\nchromatograph with a flame ionization detector (GC-FID) following established\nprotocols reported in Weinstein et al. (2016). The uncertainty associated with\nthese measurements was 5.2% based on duplicate measurements. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 737781 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1318102 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1318102 |
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 | Henrietta N Edmonds |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 51517 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Hudson Canyon Radiocarbon DIC, DIC, pH, and CH4 \n collected on cruise EN541 \n PI: John D. Kessler (University of Rochester) \n Contact: Fenix Garcia-Tigreros (University of Rochester) \n Version: 30 May 2018 |
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/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2018-05-30T16:36:11Z |
attribute | NC_GLOBAL | date_modified | String | 2019-03-15T18:45:21Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.737887.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | -72.20012 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 39.5668 |
attribute | NC_GLOBAL | geospatial_lat_min | double | 39.2878 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | -72.20012 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -72.42284 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | geospatial_vertical_max | double | 681.8 |
attribute | NC_GLOBAL | geospatial_vertical_min | double | 50.0 |
attribute | NC_GLOBAL | geospatial_vertical_positive | String | down |
attribute | NC_GLOBAL | geospatial_vertical_units | String | m |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/737887 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 737924 |
attribute | NC_GLOBAL | instruments_0_description | String | A Niskin bottle (a next generation water sampler based on the Nansen bottle) is a cylindrical, non-metallic water collection device with stoppers at both ends. The bottles can be attached individually on a hydrowire or deployed in 12, 24 or 36 bottle Rosette systems mounted on a frame and combined with a CTD. Niskin bottles are used to collect discrete water samples for a range of measurements including pigments, nutrients, plankton, etc. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0412/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 413 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | bottle Rosette |
attribute | NC_GLOBAL | instruments_1_acronym | String | AMS |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 737921 |
attribute | NC_GLOBAL | instruments_1_description | String | An AMS measures \"long-lived radionuclides that occur naturally in our environment. AMS uses a particle accelerator in conjunction with ion sources, large magnets, and detectors to separate out interferences and count single atoms in the presence of 1x1015 (a thousand million million) stable atoms, measuring the mass-to-charge ratio of the products of sample molecule disassociation, atom ionization and ion acceleration.\" AMS permits ultra low-level measurement of compound concentrations and isotope ratios that traditional alpha-spectrometry cannot provide. More from Purdue University: http://www.physics.purdue.edu/primelab/introduction/ams.html |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB17/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Accelerator Mass Spectrometer |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 527 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | W. M. Keck Carbon Cycle Accelerator Mass Spectrometry Laboratory |
attribute | NC_GLOBAL | instruments_2_acronym | String | Gas Chromatograph |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 737922 |
attribute | NC_GLOBAL | instruments_2_description | String | Instrument separating gases, volatile substances, or substances dissolved in a volatile solvent by transporting an inert gas through a column packed with a sorbent to a detector for assay. (from SeaDataNet, BODC) |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB02/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Gas Chromatograph |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 661 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | Agilent 6850 gas chromatograph |
attribute | NC_GLOBAL | instruments_3_acronym | String | Spectrometer |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 737920 |
attribute | NC_GLOBAL | instruments_3_description | String | A spectrometer is an optical instrument used to measure properties of light over a specific portion of the electromagnetic spectrum. |
attribute | NC_GLOBAL | instruments_3_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0460/ |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Spectrometer |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 667 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | CO2 cavity-ringdown spectrometer (CRDS; Picarro G1101-i) |
attribute | NC_GLOBAL | instruments_4_acronym | String | Spectrophotometer |
attribute | NC_GLOBAL | instruments_4_dataset_instrument_nid | String | 737919 |
attribute | NC_GLOBAL | instruments_4_description | String | An instrument used to measure the relative absorption of electromagnetic radiation of different wavelengths in the near infra-red, visible and ultraviolet wavebands by samples. |
attribute | NC_GLOBAL | instruments_4_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB20/ |
attribute | NC_GLOBAL | instruments_4_instrument_name | String | Spectrophotometer |
attribute | NC_GLOBAL | instruments_4_instrument_nid | String | 707 |
attribute | NC_GLOBAL | instruments_4_supplied_name | String | Agilent Cary 100 UV-Visible spectrophotometer |
attribute | NC_GLOBAL | instruments_5_acronym | String | FID |
attribute | NC_GLOBAL | instruments_5_dataset_instrument_nid | String | 737923 |
attribute | NC_GLOBAL | instruments_5_description | String | A flame ionization detector (FID) is a scientific instrument that measures the concentration of organic species in a gas stream. It is frequently used as a detector in gas chromatography. Standalone FIDs can also be used in applications such as landfill gas monitoring, fugitive emissions monitoring and internal combustion engine emissions measurement in stationary or portable instruments. |
attribute | NC_GLOBAL | instruments_5_instrument_name | String | Flame Ionization Detector |
attribute | NC_GLOBAL | instruments_5_instrument_nid | String | 644600 |
attribute | NC_GLOBAL | instruments_5_supplied_name | String | Agilent 6850 gas chromatograph with a flame ionization detector (GC-FID) |
attribute | NC_GLOBAL | keywords | String | age, altimetry, bco, bco-dmo, biological, c14, C14_DIC_age, ch3, chemical, chemistry, conductivity, cruise, Cruise_ID, ctd, CTD_hex_file, d14, d14C_DIC, data, dataset, date, density, depth, dic, dmo, earth, Earth Science > Oceans > Ocean Chemistry > pH, erddap, file, GMT_Date, GMT_Time, hex, iso, laboratory, latitude, longitude, management, ocean, oceanography, oceans, office, preliminary, pressure, reported, sal, satellite, scale, science, sea, sea_water_ph_reported_on_total_scale, seawater, sonde, station, Station_ID, temperature, time, total, water |
attribute | NC_GLOBAL | keywords_vocabulary | String | GCMD Science Keywords |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/737887/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/737887 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 39.5668 |
attribute | NC_GLOBAL | param_mapping | String | {'737887': {'Latitude': 'flag - latitude', 'depth': 'flag - depth', 'ISO_DateTime': 'flag - time', 'Longitude': 'flag - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/737887/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | University of Rochester |
attribute | NC_GLOBAL | people_0_person_name | String | John D. Kessler |
attribute | NC_GLOBAL | people_0_person_nid | String | 737785 |
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 | University of Rochester |
attribute | NC_GLOBAL | people_1_person_name | String | Fenix Garcia-Tigreros |
attribute | NC_GLOBAL | people_1_person_nid | String | 737788 |
attribute | NC_GLOBAL | people_1_role | String | Contact |
attribute | NC_GLOBAL | people_1_role_type | String | related |
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 | Shannon Rauch |
attribute | NC_GLOBAL | people_2_person_nid | String | 51498 |
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 | Aerobic methane oxidation |
attribute | NC_GLOBAL | projects_0_acronym | String | Aerobic methane oxidation |
attribute | NC_GLOBAL | projects_0_description | String | NSF Award Abstract:\nRoughly 8 billion moles of methane (CH4) were emitted in 83 days during the Deepwater Horizon disaster in the northern Gulf of Mexico in 2010. Interestingly, none of this CH4 was emitted to the atmosphere, but instead stayed dissolved and suspended as \"plume\" or \"intrusion\" layers approximately 1000m below the ocean surface. Based on measurements of CH4 concentration and oxidation rates, dissolved oxygen anomalies, and microbial community structure as well as a CH4 geochemical model, it was determined that all the CH4 emitted during this disaster was respired within 120 days of the initial well blowout. In addition, the methanotrophic bacteria responsible for the oxidation of this CH4 appeared to experience all stages of microbial growth, limited only by the availability of CH4. This finding suggests that releases of CH4 into deepwater, be them anthropogenic or natural, will have minimal direct influence on the radiative budget of the atmosphere.\nThe major weakness in these previous investigations is that CH4 related parameters were only measured at the beginning (May - June 2010) and end (September - October 2010) of this massive CH4 feast, primarily because the rapid demise of CH4 was unanticipated. Thus, the time- and growth phase-dependent understanding of the kinetics of this bloom response is only based on model interpolation between endpoints. A more complete, and measurement-based, understanding of the chemical kinetics is necessary to predict an oceanographic environment's ability to respire large CH4 perturbations. And while measurements of CH4 stable isotopes in theory can be used to assess the extent that the released CH4 has been oxidized, this kinetic isotope effect can only be used in a quantitative fashion if it is known how the isotopic fractionation factor changes with varying chemical and temperature conditions and throughout all stages of the microbial bloom.\nIn this study, researchers at the Texas A & M University will test two fundamental hypotheses relating to aerobic CH4 oxidation and ultimately produce a thorough characterization of the time-, growth phase-, and temperature-dependency of CH4 oxidation rates, oxidation rate constants, and isotopic fractionation factors. Hypothesis 1: Excluding mixing processes, the bacterial response to a large CH4 perturbation will be limited primarily by the availability of CH4 or dissolved oxygen. Hypothesis 2: Without knowing the stage of microbial growth, measurements of natural stable isotopes of CH4 and dissolved carbon (organic and/or inorganic) cannot be used to assess the extent of CH4 oxidation in situations of large CH4 perturbations. In order to test these hypotheses, with the goal of disproving hypothesis 2, a suite of mesocosm and pure culture incubations will be conducted. Throughout these incubations, concentrations of CH4 and dissolved inorganic carbon as well as their 13C isotopes will be measured in extremely high resolution with new equipment and experimental designs. In addition, dissolved oxygen, nutrient concentrations, trace metals, CH4 oxidation rates, and microbial community structure will be measured.\nBroader Impacts. In addition to the normal dissemination of results in publications, meeting presentations, and on a project web site, this work will have strong educational and research impacts with close interactions between the PIs, postdoctoral scholar, graduate student, and undergraduate researchers with collaborations between Texas A&M University and the University of California Santa Barbara. The students will have extended visits at each lab for skill development, knowledge transfer, and general academic growth. During 2010, an informal collaboration was established with Ms. Vicki Soutar, a high school science teacher in Watkinsville, GA, to develop high school science laboratory exercises using real scientific data. This proposed project will involve Ms. Soutar to formalize, enhance, extend, and disseminate the products of this collaboration |
attribute | NC_GLOBAL | projects_0_end_date | String | 2016-02 |
attribute | NC_GLOBAL | projects_0_name | String | Investigating the chemical and isotopic kinetics of aerobic methane oxidation |
attribute | NC_GLOBAL | projects_0_project_nid | String | 737782 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2012-12 |
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 | 39.2878 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | subsetVariables | String | Cruise_ID |
attribute | NC_GLOBAL | summary | String | Radiocarbon DIC, DIC concentration, pH, and [CH4] in Hudson Canyon, northern US Atlantic Margin collected from R/V Endeavor cruise EN541 in July 2014. |
attribute | NC_GLOBAL | time_coverage_end | String | 2014-07-13T01:43:43Z |
attribute | NC_GLOBAL | time_coverage_start | String | 2014-07-09T14:46:14Z |
attribute | NC_GLOBAL | title | String | [Hudson Canyon DIC and pH] - Radiocarbon DIC, DIC concentration, pH, and [CH4] in Hudson Canyon, northern US Atlantic Margin collected from R/V Endeavor cruise EN541 in July 2014 (Investigating the chemical and isotopic kinetics of aerobic methane oxidation) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -72.42284 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | Cruise_ID | String | ||
attribute | Cruise_ID | bcodmo_name | String | cruise_id |
attribute | Cruise_ID | description | String | Cruise identifier (EN = R/V Endeavor) |
attribute | Cruise_ID | long_name | String | Cruise ID |
attribute | Cruise_ID | units | String | unitless |
variable | CTD_hex_file | String | ||
attribute | CTD_hex_file | bcodmo_name | String | cast |
attribute | CTD_hex_file | description | String | CTD hex file name |
attribute | CTD_hex_file | long_name | String | CTD Hex File |
attribute | CTD_hex_file | units | String | untiless |
variable | Station_ID | String | ||
attribute | Station_ID | bcodmo_name | String | station |
attribute | Station_ID | description | String | Cruise station identifier |
attribute | Station_ID | long_name | String | Station ID |
attribute | Station_ID | units | String | unitless |
variable | GMT_Date | String | ||
attribute | GMT_Date | bcodmo_name | String | date_gmt |
attribute | GMT_Date | description | String | Date GMT (yyyy-mm-dd) |
attribute | GMT_Date | long_name | String | GMT Date |
attribute | GMT_Date | time_precision | String | 1970-01-01 |
attribute | GMT_Date | units | String | unitless |
variable | time | double | ||
attribute | time | _CoordinateAxisType | String | Time |
attribute | time | actual_range | double | 1.404917174E9, 1.405215823E9 |
attribute | time | axis | String | T |
attribute | time | bcodmo_name | String | ISO_DateTime_UTC |
attribute | time | description | String | Date and time formatted to ISO8601 standard: yyyy-mm-ddTHH:MM:SS |
attribute | time | ioos_category | String | Time |
attribute | time | long_name | String | ISO Date Time |
attribute | time | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/DTUT8601/ |
attribute | time | source_name | String | ISO_DateTime |
attribute | time | standard_name | String | time |
attribute | time | time_origin | String | 01-JAN-1970 00:00:00 |
attribute | time | time_precision | String | 1970-01-01T00:00:00Z |
attribute | time | units | String | seconds since 1970-01-01T00:00:00Z |
variable | GMT_Time | String | ||
attribute | GMT_Time | bcodmo_name | String | time_gmt |
attribute | GMT_Time | description | String | Time GMT (HH:MM:SS) |
attribute | GMT_Time | long_name | String | GMT Time |
attribute | GMT_Time | units | String | unitless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | 39.2878, 39.5668 |
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 | Latitude North at start of CTD cast |
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/ |
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 | -72.42284, -72.20012 |
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 | Longitude West at start of CTD cast |
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/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | depth | double | ||
attribute | depth | _CoordinateAxisType | String | Height |
attribute | depth | _CoordinateZisPositive | String | down |
attribute | depth | _FillValue | double | NaN |
attribute | depth | actual_range | double | 50.0, 681.8 |
attribute | depth | axis | String | Z |
attribute | depth | bcodmo_name | String | depth |
attribute | depth | colorBarMaximum | double | 8000.0 |
attribute | depth | colorBarMinimum | double | -8000.0 |
attribute | depth | colorBarPalette | String | TopographyDepth |
attribute | depth | description | String | Niskin bottle depth (m) at sample collection |
attribute | depth | ioos_category | String | Location |
attribute | depth | long_name | String | Depth |
attribute | depth | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/DEPH/ |
attribute | depth | positive | String | down |
attribute | depth | standard_name | String | depth |
attribute | depth | units | String | m |
variable | pressure | float | ||
attribute | pressure | _FillValue | float | NaN |
attribute | pressure | actual_range | float | 50.4, 688.2 |
attribute | pressure | bcodmo_name | String | pressure |
attribute | pressure | description | String | Pressure at sample collection |
attribute | pressure | long_name | String | Pressure |
attribute | pressure | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PRESPR01/ |
attribute | pressure | units | String | Digiquartz (db) |
variable | temp | float | ||
attribute | temp | _FillValue | float | NaN |
attribute | temp | actual_range | float | 5.27, 18.35 |
attribute | temp | bcodmo_name | String | temperature |
attribute | temp | description | String | Temperature at sample collection |
attribute | temp | long_name | String | Temperature |
attribute | temp | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/TEMPP901/ |
attribute | temp | units | String | Degrees Celsius |
variable | sal | float | ||
attribute | sal | _FillValue | float | NaN |
attribute | sal | actual_range | float | 35.01, 36.05 |
attribute | sal | bcodmo_name | String | sal |
attribute | sal | description | String | Salinity at sample collection |
attribute | sal | long_name | String | Sal |
attribute | sal | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PSALST01/ |
attribute | sal | units | String | Practical (PSU) |
variable | Density | double | ||
attribute | Density | _FillValue | double | NaN |
attribute | Density | actual_range | double | 1025.87, 1030.82 |
attribute | Density | bcodmo_name | String | density |
attribute | Density | description | String | Density at sample collection |
attribute | Density | long_name | String | Density |
attribute | Density | units | String | kilograms per cubic meter (Kg/m^3) |
variable | pH | float | ||
attribute | pH | _FillValue | float | NaN |
attribute | pH | actual_range | float | 7.7873, 8.0595 |
attribute | pH | bcodmo_name | String | pH |
attribute | pH | colorBarMaximum | double | 9.0 |
attribute | pH | colorBarMinimum | double | 7.0 |
attribute | pH | description | String | Spectrophotometric pH measured at 25 C using the total hydrogen ion scale |
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/ |
attribute | pH | units | String | Unitless; pH scale |
variable | DIC | float | ||
attribute | DIC | _FillValue | float | NaN |
attribute | DIC | actual_range | float | 1319.47, 2259.43 |
attribute | DIC | bcodmo_name | String | DIC |
attribute | DIC | description | String | Dissolved Inorganic Carbon concentration |
attribute | DIC | long_name | String | DIC |
attribute | DIC | units | String | micromoles per kilogram (umol/kg) |
variable | CH3 | float | ||
attribute | CH3 | _FillValue | float | NaN |
attribute | CH3 | actual_range | float | 1.97, 334.68 |
attribute | CH3 | bcodmo_name | String | CH4 |
attribute | CH3 | description | String | Dissolved methane concentration |
attribute | CH3 | long_name | String | CH3 |
attribute | CH3 | units | String | nanomolar (nM) |
variable | d14C_DIC | float | ||
attribute | d14C_DIC | _FillValue | float | NaN |
attribute | d14C_DIC | actual_range | float | -28.5, 41.8 |
attribute | d14C_DIC | bcodmo_name | String | unknown |
attribute | d14C_DIC | description | String | Natural radiocarbon of DIC |
attribute | d14C_DIC | long_name | String | D14 C DIC |
attribute | d14C_DIC | units | String | Per mil (‰) |
variable | C14_DIC_age | String | ||
attribute | C14_DIC_age | bcodmo_name | String | unknown |
attribute | C14_DIC_age | description | String | Age of DIC |
attribute | C14_DIC_age | long_name | String | C14 DIC Age |
attribute | C14_DIC_age | units | String | Years before present |