BCO-DMO ERDDAP
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Row Type | Variable Name | Attribute Name | Data Type | Value |
---|---|---|---|---|
attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson |
attribute | NC_GLOBAL | acquisition_description | String | NO3-+NO2- d15N analysis was by the \\u201cdenitrifier method\\u201d and followed\nthe methods described by Sigman et al., 2001, Casciotti et al., 2002, McIlvin\nand Casciotti, 2011, and Weigand et al., 2016. Briefly, NO3-+NO2- was\nquantitatively reduced to N2O by Pseudomonas aureofaciens and Pseudomonas\nchlororaphis, which was then cryogenically focused and analyzed on an isotope\nratio mass spectrometer. A volume of sample was added to each bacterial vial\nto achieve a final quantity of 10 or 20 nmols N2O, which was then purged from\nthe vial using a helium carrier gas. The d15N of N2O in samples was calibrated\nwith the international isotopic reference materials described in the\nProcessing Description. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 710561 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1537314 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1537314 |
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 | Station location and NO3+NO2 d15N values measured for the OUTPACE long duration (LD) stations. \n PI: Angela Knapp \n Version: 2018-04-11 |
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 | 2018-04-11T19:49:07Z |
attribute | NC_GLOBAL | date_modified | String | 2018-09-20T17:38:55Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.733303 |
attribute | NC_GLOBAL | Easternmost_Easting | double | 168.0118 |
attribute | NC_GLOBAL | geospatial_lat_max | double | -18.179 |
attribute | NC_GLOBAL | geospatial_lat_min | double | -19.9832 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | 168.0118 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -172.7813 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | geospatial_vertical_max | double | 2002.0 |
attribute | NC_GLOBAL | geospatial_vertical_min | double | 3.0 |
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/733237 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | IR Mass Spec |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Nitrate+nitrite d15N was measured using a Thermo Finnigan Delta V isotope ratio mass spectrometer. |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 733270 |
attribute | NC_GLOBAL | instruments_0_description | String | The Isotope-ratio Mass Spectrometer is a particular type of mass spectrometer used to measure the relative abundance of isotopes in a given sample (e.g. VG Prism II Isotope Ratio Mass-Spectrometer). |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB16/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Isotope-ratio Mass Spectrometer |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 469 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Thermo Finnigan Delta V isotope ratio mass spectrometer. |
attribute | NC_GLOBAL | keywords | String | bco, bco-dmo, biological, cast, chemical, d15, data, dataset, date, density, depth, dmo, earth, Earth Science > Oceans > Salinity/Density > Density, erddap, latitude, longitude, management, nitrate, nitrite, no2, no3, NO3_NO2, NO3_NO2_d15N, NO3_NO2_d15N_1_SD, ocean, oceanography, oceans, office, preliminary, salinity, science, sea, sea_water_sigma_theta, seawater, sigma, Sigma_theta, station, theta, water |
attribute | NC_GLOBAL | keywords_vocabulary | String | GCMD Science Keywords |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/733237/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/733237 |
attribute | NC_GLOBAL | Northernmost_Northing | double | -18.179 |
attribute | NC_GLOBAL | param_mapping | String | {'733237': {'Latitude': 'flag - latitude', 'Depth': 'flag - depth', 'Longitude': 'flag - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/733237/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | Florida State University |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | FSU |
attribute | NC_GLOBAL | people_0_person_name | String | Angela N. Knapp |
attribute | NC_GLOBAL | people_0_person_nid | String | 555499 |
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 | Mediterranean Institute of Oceanography |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | MIO |
attribute | NC_GLOBAL | people_1_person_name | String | Sophie Bonnet |
attribute | NC_GLOBAL | people_1_person_nid | String | 663895 |
attribute | NC_GLOBAL | people_1_role | String | International Collaborator |
attribute | NC_GLOBAL | people_1_role_type | String | originator |
attribute | NC_GLOBAL | people_2_affiliation | String | Mediterranean Institute of Oceanography |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | MIO |
attribute | NC_GLOBAL | people_2_person_name | String | Thierry Moutin |
attribute | NC_GLOBAL | people_2_person_nid | String | 663893 |
attribute | NC_GLOBAL | people_2_role | String | International Collaborator |
attribute | NC_GLOBAL | people_2_role_type | String | originator |
attribute | NC_GLOBAL | people_3_affiliation | String | Mediterranean Institute of Oceanography |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | MIO |
attribute | NC_GLOBAL | people_3_person_name | String | Oliver Grosso |
attribute | NC_GLOBAL | people_3_person_nid | String | 733295 |
attribute | NC_GLOBAL | people_3_role | String | Scientist |
attribute | NC_GLOBAL | people_3_role_type | String | originator |
attribute | NC_GLOBAL | people_4_affiliation | String | Villefranche Oceanographic Laboratory |
attribute | NC_GLOBAL | people_4_affiliation_acronym | String | LOV |
attribute | NC_GLOBAL | people_4_person_name | String | Nathalie Leblond |
attribute | NC_GLOBAL | people_4_person_nid | String | 733296 |
attribute | NC_GLOBAL | people_4_role | String | Scientist |
attribute | NC_GLOBAL | people_4_role_type | String | originator |
attribute | NC_GLOBAL | people_5_affiliation | String | Florida State University |
attribute | NC_GLOBAL | people_5_affiliation_acronym | String | FSU |
attribute | NC_GLOBAL | people_5_person_name | String | Kelly M. McCabe |
attribute | NC_GLOBAL | people_5_person_nid | String | 733294 |
attribute | NC_GLOBAL | people_5_role | String | Student |
attribute | NC_GLOBAL | people_5_role_type | String | related |
attribute | NC_GLOBAL | people_6_affiliation | String | Florida State University |
attribute | NC_GLOBAL | people_6_affiliation_acronym | String | FSU |
attribute | NC_GLOBAL | people_6_person_name | String | Angela N. Knapp |
attribute | NC_GLOBAL | people_6_person_nid | String | 555499 |
attribute | NC_GLOBAL | people_6_role | String | Contact |
attribute | NC_GLOBAL | people_6_role_type | String | related |
attribute | NC_GLOBAL | people_7_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_7_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_7_person_name | String | Mathew Biddle |
attribute | NC_GLOBAL | people_7_person_nid | String | 708682 |
attribute | NC_GLOBAL | people_7_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_7_role_type | String | related |
attribute | NC_GLOBAL | project | String | SW Pac N2 fixation |
attribute | NC_GLOBAL | projects_0_acronym | String | SW Pac N2 fixation |
attribute | NC_GLOBAL | projects_0_description | String | NSF Award Abstract:\nThe availability of nitrogen in the surface ocean plays a critical role regulating rates of primary productivity in the ocean, and thus through modification of the carbon cycle, nitrogen has the capacity to influence climate. The dominant source of biologically available nitrogen to the ocean is through a process known as di-nitrogen (N2) fixation, which involves the reduction of N2 gas dissolved in seawater to ammonium by microbes referred to as diazotrophs. While significant progress has been made identifying a diversity of marine diazotrophs in recent years using molecular tools, quantifying global rates of N2 fixation, and identifying which ocean basin supports the highest fluxes, has remained a vexing question. This research will quantify rates of N2 fixation as well as its importance for supporting production in the southwest Pacific Ocean. Results from this research will shed light on the sensitivities of N2 fixation (temperature, iron concentrations) as well as the extent of spatial and temporal coupling of nitrogen sources and sinks in the ocean. The work will be carried out by an early career scientist, and involve mentoring of young women, middle school girls and minorities, training of undergraduate and graduate researchers, and international collaborations.\nIdentifying the spatial distribution of the largest di-nitrogen (N2) fixation fluxes to the ocean remains a critical goal of chemical oceanography. The spatial distribution can inform our understanding of the environmental sensitivities of N2 fixation and the capacity for the dominant marine nitrogen (N) source and sink processes to respond to each other and thus influence the global carbon cycle and climate. In addition to temperature, two factors are at the heart of the current debate over what influences the spatial distribution of N2 fixation in the ocean: 1) the presence of adequate iron to meet the needs of N2 fixing microbes, and, 2) the absolute concentrations as well as ratios of surface ocean nitrate and phosphate concentrations that are low relative to the \"Redfield\" ratio, which are thought to favor N2 fixing microbes. This project will test the effects of gradients in atmospheric dust deposition on N2 fixation rates when surface waters have relatively constant but favorable nitrate to phosphate concentrations. The work will be carried out in the southwest Pacific, a region highlighted by new modeling work for its unique geochemical characteristics that are expected to favor significant N2 fixation fluxes. Nitrate+nitrite d15N as well as total dissolved nitrogen (TDN) concentration and d15N will be measured in water column samples collected on a French cruise and sediment traps were deployed to capture the sinking particulate N flux. The results will be compared with published work to evaluate which ocean regions support the largest N2 fixation fluxes.\nMore information:\nThis project was part of the Oligotrophy to UlTra-oligotrophy PACific Experiment (OUTPACE) cruise in the Southwest Pacific between New Caledonia (166°28' E; 22°14' S) and Tahiti (149°36' W; 17°34' S) 0-2000 m\n* OUTPACE cruise (doi: https://dx.doi.org/10.17600/15000900)\n* OUTPACE website: https://outpace.mio.univ-amu.fr/?lang=en |
attribute | NC_GLOBAL | projects_0_end_date | String | 2018-07 |
attribute | NC_GLOBAL | projects_0_geolocation | String | Southwest Pacific Ocean between New Caledonia and Tahiti along ~18 deg S |
attribute | NC_GLOBAL | projects_0_name | String | Quantifying nitrogen fixation along unique geochemical gradients in the southwest Pacific Ocean |
attribute | NC_GLOBAL | projects_0_project_nid | String | 710562 |
attribute | NC_GLOBAL | projects_0_project_website | String | http://scope.soest.hawaii.edu/data/lava/lava.html |
attribute | NC_GLOBAL | projects_0_start_date | String | 2015-08 |
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 | -19.9832 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | summary | String | Constraining the rates and spatial distribution of di-nitrogen (N2) fixation fluxes to the ocean informs our understanding of the environmental sensitivities of N2 fixation as well as the timescale over which the fluxes of nitrogen (N) to and from the ocean may respond to each other. Here we quantify rates of N2 fixation as well as its contribution to export production along a zonal transect in the Western Tropical South Pacific (WTSP) Ocean using N isotope (\\u201cd15N\\u201d) budgets. Comparing measurements of water column nitrate+nitrite d15N with the d15N of sinking particulate N at a western, central, and eastern station, these d15N budgets indicate high, modest, and low rates of N2 fixation at the respective stations. The results also imply that N2 fixation supports exceptionally high, i.e., >50%, of export production at the western and central stations, which are also proximal to the largest iron sources. These geochemically-based rates of N2 fixation are equal to or greater than those previously reported in the tropical North Atlantic, indicating that the WTSP Ocean has the capacity to support globally significant rates of N2 fixation, which may compensate for N removal in the oxygen deficient zones of the eastern tropical Pacific. |
attribute | NC_GLOBAL | title | String | [OUTPACE - water column nitrate+nitrite] - Water column nitrate+nitrite d15N measurements from R/V L'Atalante in the southwest Pacific Ocean between New Caledonia and Tahiti from February to March 2015 (Quantifying nitrogen fixation along unique geochemical gradients in the southwest Pacific Ocean) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -172.7813 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | Date | int | ||
attribute | Date | _FillValue | int | 2147483647 |
attribute | Date | actual_range | int | 20150223, 20150330 |
attribute | Date | bcodmo_name | String | date |
attribute | Date | description | String | Date of observation in four digit year; 2 digit month; 2 digit day (yyyymmdd) format |
attribute | Date | long_name | String | Date |
attribute | Date | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/ADATAA01/ |
attribute | Date | units | String | unitless |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | -172.7813, 168.0118 |
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 with west 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/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | -19.9832, -18.179 |
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 with south 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/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | Station | String | ||
attribute | Station | bcodmo_name | String | station |
attribute | Station | description | String | name of the station |
attribute | Station | long_name | String | Station |
attribute | Station | units | String | unitless |
variable | Cast | short | ||
attribute | Cast | _FillValue | short | 32767 |
attribute | Cast | actual_range | short | 10, 210 |
attribute | Cast | bcodmo_name | String | cast |
attribute | Cast | description | String | cast number |
attribute | Cast | long_name | String | Cast |
attribute | Cast | units | String | unitless |
variable | depth | double | ||
attribute | depth | _CoordinateAxisType | String | Height |
attribute | depth | _CoordinateZisPositive | String | down |
attribute | depth | _FillValue | double | NaN |
attribute | depth | actual_range | double | 3.0, 2002.0 |
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 | depth of observation |
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 | Sigma_theta | float | ||
attribute | Sigma_theta | _FillValue | float | NaN |
attribute | Sigma_theta | actual_range | float | 21.71, 27.67 |
attribute | Sigma_theta | bcodmo_name | String | sigma_theta |
attribute | Sigma_theta | description | String | potential density |
attribute | Sigma_theta | long_name | String | Sea Water Sigma Theta |
attribute | Sigma_theta | units | String | kilograms per meter cubed (kg/m3) |
variable | NO3_NO2 | String | ||
attribute | NO3_NO2 | bcodmo_name | String | NO3_NO2 |
attribute | NO3_NO2 | description | String | nitrate+nitrite concentration ([NO3-+NO2-]) |
attribute | NO3_NO2 | long_name | String | NO3 NO2 |
attribute | NO3_NO2 | units | String | micromole (uM) |
variable | NO3_NO2_d15N | String | ||
attribute | NO3_NO2_d15N | bcodmo_name | String | 15N of nitrate plus nitrite |
attribute | NO3_NO2_d15N | description | String | nitrate+nitrite d15N (NO3-+NO2- d15N) |
attribute | NO3_NO2_d15N | long_name | String | NO3 NO2 D15 N |
attribute | NO3_NO2_d15N | units | String | per mil |
variable | NO3_NO2_d15N_1_SD | String | ||
attribute | NO3_NO2_d15N_1_SD | bcodmo_name | String | 15N of nitrate plus nitrite |
attribute | NO3_NO2_d15N_1_SD | description | String | nitrate+nitrite d15N standard deviation |
attribute | NO3_NO2_d15N_1_SD | long_name | String | NO3 NO2 D15 N 1 SD |
attribute | NO3_NO2_d15N_1_SD | units | String | per mil |