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| Dataset Title: | (SECOORA) Glider - ECOA1 - ECOA1 Discrete Sampling: Dissolved inorganic carbon, total alkalinity, pH, nutrients and other variables collected from profile and discrete sample observations using CTD, Niskin bottle, and other instruments from NOAA Ship Gordon Gunter off the U.S. East Coast during the East Coast Ocean Acidification (GU-15-04 ECOA1) from 2015-06-20 to 2015-07- 23 (NCEI Accession 0159428). 
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| Institution: | NOAA OAP (Dataset ID: axiom-netcdf-harvest-socan-GU-15-04-ECOA1-1434765195-1437670876) |
| Range: | longitude = -80.9735 to -61.72616°E, latitude = 26.98217 to 44.9445°N, time = 2015-06-20T01:53:15Z to 2015-07-23T16:43:13Z |
| Information: | Summary
| License
| FGDC
| ISO 19115
| Metadata
| Background
| Subset
| Data Access Form
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Attributes {
s {
cdom {
Float32 _FillValue -9999.9;
Float32 actual_range -1.975172e-7, 4.101363e-4;
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String detailed_sampling_and_analyzing_information "Typically three depths (surface, mix layer, and depth inbetween) are sampled via niskin bottler. The samples were filtered under a gentle vacuum (<5 in Hg) through pre-combusted (6 hours at 450 degree C) 47mm GFF filters and separated into 2 or 3 (depending on depth) 40ml vials for DOC and one 125ml bottle for CDOM. The DOC vials were frozen and the CDOM bottles refrigerated. DOC and CDOM samples were analyzed by Antonio Mannino’s laboratory at NASA Goddard.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Concentration Of Colored Dissolved Organic Matter";
String method_reference "Mannino, A., M. E. Russ, and S. B. Hooker (2008), Algorithm development and validation for satellite-derived distributions of DOC and CDOM in the U.S. Middle Atlantic Bight, J. Geophys. Res., 113, C07051, doi:10.1029/2007JC004493";
Float32 missing_value -9999.9;
String observation_type "Profile";
String parameter_id "360";
String researcher_institution "NASA Goddard Space Flight Center";
String researcher_name "Antonio Mannino";
String sampling_instrument "Niskin bottle";
String standard_name "concentration_of_colored_dissolved_organic_matter_in_sea_water_expressed_as_equivalent_mass_fraction_of_quinine_sulfate_dihydrate";
String unit_id "3";
String units "1";
String variable_type "In-situ observation";
}
chl_a {
Float32 _FillValue -9999.9;
Float32 actual_range 0.046, 8.324;
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String detailed_sampling_and_analyzing_information "Samples were taken with a niskin bottle from the surface, mix layer, and where applicable at a third depth between the surface and mix layer. The samples were run through precombusted (6 hours at 450 degree C) 25mm GFF filters, placed in precombusted aluminum foil, and stored in liquid nitrogen until analysis.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Chlorophyll a";
String method_reference "Van Heukelem, L. and C.S. Thomas, 2001: Computer-assisted high-performance liquid chromatography method development with applications to the isolation and analysis of phytoplankton pigments. J.Chromatogr. A, 910, 31-49.";
Float32 missing_value -9999.9;
String parameter_id "427";
String researcher_institution "NASA Goddard Space Flight Center";
String researcher_name "Antonio Mannino";
String sampling_instrument "Niskin bottle";
String standard_name "mass_concentration_of_chlorophyll_a_in_sea_water";
String unit_id "17";
String units "kg.m-3";
String variable_type "In-situ observation";
}
latitude {
String _CoordinateAxisType "Lat";
Float32 _FillValue -9999.9;
Float32 actual_range 26.98217, 44.9445;
String axis "Y";
String ioos_category "Location";
String long_name "Profile Location";
Float32 missing_value -9999.9;
String standard_name "latitude";
String units "degrees_north";
Float32 valid_max 90.0;
Float32 valid_min -90.0;
}
longitude {
String _CoordinateAxisType "Lon";
Float32 _FillValue -9999.9;
Float32 actual_range -80.9735, -61.72616;
String axis "X";
String ioos_category "Location";
String long_name "Profile Location";
Float32 missing_value -9999.9;
String standard_name "longitude";
String units "degrees_east";
Float32 valid_max 180.0;
Float32 valid_min -180.0;
}
nitrate {
Float32 _FillValue -9999.9;
Float32 actual_range 0.0, 32.82;
String analyzing_instrument "Continuous flow analyzer (CFA) using the standard and analysis protocols for the WOCE hydrographic program as set forth in the manual by L.I. Gordon, et al. (1993).";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Nutrient samples were collected from Niskin bottles, after at least three seawater rinses. Sample analysis typically began within a few hours of sample collection after the samples had warmed to room temperature. Those samples not analyzed within 3 hours were refrigerated for later analysis. Samples were analyzed for phosphate (PO4- 3), nitrate (NO3-), nitrite (NO2-) and orthosilicic acid (H4SiO4). Samples for nitrate analysis were passed through a cadmium column, which reduced nitrate to nitrite, and the resulting nitrite concentration (i.e. the sum of nitrate + nitrite which is signified as N+N) was then determined as described above. Nitrate concentrations were determined from the difference of N+N and nitrite.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Nitrate Per Unit Mass In Sea Water";
String method_reference "Armstrong, F.A.J., Stearns, C.R. and Strickland, J.D.H. (1967). The measurement of upwelling and subsequent biological processes by means of the Technicon AutoAnalyzer and associated equipment. Deep-Sea Res. 14:381-389. Gordon, L.I., Jennings Jr., J.C., Ross, A.A. and Krest, J.M. (1993). A suggested protocol for the continuous automated analysis of seawater nutrients (phosphate, nitrate, nitrite and silicic acid) in the WOCE Hydrographic program and the Joint Global Ocean Fluxes Study. WOCE Operations Manual, vol. 3: The Observational Programme, Section 3.2: WOCE Hydrographic Programme, Part 3.1.3: WHP Operations and Methods. WHP Office Report WHPO 91-1; WOCE Report No. 68/91. November 1994, Revision 1, Woods Hole, MA., USA, 52 loose-leaf pages.";
Float32 missing_value -9999.9;
String observation_type "Profile and surface underway";
String parameter_id "130";
String researcher_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String researcher_name "Jia-Zhong Zhang";
String sampling_instrument "Niskin bottle and flow through pump";
String standard_name "nitrate";
String uncertainty "A mixed stock standard consisting of silicic acid, phosphate and nitrate was prepared by dissolving high purity standard materials (KNO3, KH2PO4 and Na2SiF6) in deionized water using a two step dilution for phosphate and nitrate. This standard was stored at room temperature. A nitrite stock standard was prepared dissolving NaNO2 in distilled water, and this standard was stored in a refrigerator on the ship. Working standards were prepared fresh daily by diluting the stock solutions in low nutrient seawater. The mixed standards were verified against commercial standards, and in-lab standards.";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
nitrate_nitrite {
Float32 _FillValue -9999.9;
Float32 actual_range 0.0, 32.83;
String analyzing_instrument "Continuous flow analyzer (CFA) using the standard and analysis protocols for the WOCE hydrographic program as set forth in the manual by L.I. Gordon, et al. (1993).";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Nutrient samples were collected from Niskin bottles, after at least three seawater rinses. Sample analysis typically began within a few hours of sample collection after the samples had warmed to room temperature. Those samples not analyzed within 3 hours were refrigerated for later analysis. Samples were analyzed for phosphate (PO4- 3), nitrate (NO3-), nitrite (NO2-) and orthosilicic acid (H4SiO4). Samples were passed through a cadmium column, which reduced nitrate to nitrite, and the resulting nitrite concentration (i.e. the sum of nitrate + nitrite which is signified as N+N) was then determined as described above.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Nitrate And Nitrite Per Unit Mass In Sea Water";
String method_reference "Armstrong, F.A.J., Stearns, C.R. and Strickland, J.D.H. (1967). The measurement of upwelling and subsequent biological processes by means of the Technicon AutoAnalyzer and associated equipment. Deep-Sea Res. 14:381-389. Gordon, L.I., Jennings Jr., J.C., Ross, A.A. and Krest, J.M. (1993). A suggested protocol for the continuous automated analysis of seawater nutrients (phosphate, nitrate, nitrite and silicic acid) in the WOCE Hydrographic program and the Joint Global Ocean Fluxes Study. WOCE Operations Manual, vol. 3: The Observational Programme, Section 3.2: WOCE Hydrographic Programme, Part 3.1.3: WHP Operations and Methods. WHP Office Report WHPO 91-1; WOCE Report No. 68/91. November 1994, Revision 1, Woods Hole, MA., USA, 52 loose-leaf pages.";
Float32 missing_value -9999.9;
String observation_type "Profile and surface underway";
String researcher_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String researcher_name "Jia-Zhong Zhang";
String sampling_instrument "Niskin bottle and flow through pump";
String standard_name "moles_of_nitrate_and_nitrite_per_unit_mass_in_sea_water";
String uncertainty "A mixed stock standard consisting of silicic acid, phosphate and nitrate was prepared by dissolving high purity standard materials (KNO3, KH2PO4 and Na2SiF6) in deionized water using a two step dilution for phosphate and nitrate. This standard was stored at room temperature. A nitrite stock standard was prepared dissolving NaNO2 in distilled water, and this standard was stored in a refrigerator on the ship. Working standards were prepared fresh daily by diluting the stock solutions in low nutrient seawater. The mixed standards were verified against commercial standards, and in-lab standards.";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
nitrite {
Float32 _FillValue -9999.9;
Float32 actual_range 0.0, 0.5;
String analyzing_instrument "Continuous flow analyzer (CFA) using the standard and analysis protocols for the WOCE hydrographic program as set forth in the manual by L.I. Gordon, et al. (1993).";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Nutrient samples were collected from Niskin bottles, after at least three seawater rinses. Sample analysis typically began within a few hours of sample collection after the samples had warmed to room temperature. Those samples not analyzed within 3 hours were refrigerated for later analysis. Samples were analyzed for phosphate (PO4- 3), nitrate (NO3-), nitrite (NO2-) and orthosilicic acid (H4SiO4). Nitrite was determined by diazotizing the sample with sulfanilamide and coupling with N-1 naphthyl ethylenediamine dihydrochloride to form an azo dye. The color produced is measured at 540 nm.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Nitrite Per Unit Mass In Sea Water";
String method_reference "Armstrong, F.A.J., Stearns, C.R. and Strickland, J.D.H. (1967). The measurement of upwelling and subsequent biological processes by means of the Technicon AutoAnalyzer and associated equipment. Deep-Sea Res. 14:381-389. Gordon, L.I., Jennings Jr., J.C., Ross, A.A. and Krest, J.M. (1993). A suggested protocol for the continuous automated analysis of seawater nutrients (phosphate, nitrate, nitrite and silicic acid) in the WOCE Hydrographic program and the Joint Global Ocean Fluxes Study. WOCE Operations Manual, vol. 3: The Observational Programme, Section 3.2: WOCE Hydrographic Programme, Part 3.1.3: WHP Operations and Methods. WHP Office Report WHPO 91-1; WOCE Report No. 68/91. November 1994, Revision 1, Woods Hole, MA., USA, 52 loose-leaf pages.";
Float32 missing_value -9999.9;
String observation_type "Profile and surface underway";
String parameter_id "423";
String researcher_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String researcher_name "Jia-Zhong Zhang";
String sampling_instrument "Niskin bottle and flow through pump";
String standard_name "nitrite";
String uncertainty "A mixed stock standard consisting of silicic acid, phosphate and nitrate was prepared by dissolving high purity standard materials (KNO3, KH2PO4 and Na2SiF6) in deionized water using a two step dilution for phosphate and nitrate. This standard was stored at room temperature. A nitrite stock standard was prepared dissolving NaNO2 in distilled water, and this standard was stored in a refrigerator on the ship. Working standards were prepared fresh daily by diluting the stock solutions in low nutrient seawater. The mixed standards were verified against commercial standards, and in-lab standards.";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
nitrogen {
Float32 _FillValue -9999.9;
Float32 actual_range 6.434762e-6, 2.124023e-4;
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String detailed_sampling_and_analyzing_information "Typically three depths (surface, mix layer, and depth inbetween) are sampled via niskin bottle. POC/PN samples are collected in 0.5, 1.04 or 2.2 Liter, brown polypropylene bottles. Samples are filtered on precombusted Whatman GF/F 25mm under low vacuum pressure (40 mm Hg) Filter is removed, folded in half with the particulate part inside the fold and wrapped in precombusted aluminum foil. Samples are stored in Liquid Nitrogen and transferred post cruise to a -80 C freezer until processed.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Mass Concentration Of Organic Detritus Expressed as Nitrogen In Sea Water";
String method_reference "Hedges, J.I. and J.H. Stern. 1984. Carbon and nitrogen determinations of carbonate-containing solids. Limnol. Oceanogr. 29: 657-663.";
Float32 missing_value -9999.9;
String parameter_id "440";
String researcher_institution "NASA Goddard Space Flight Center";
String researcher_name "Antonio Mannino";
String standard_name "mass_concentration_total_dissolved_nitrogen";
String unit_id "17";
String units "kg.m-3";
}
oxygen_concentration {
Float32 _FillValue -9999.9;
Float32 actual_range 98.837, 371.594;
String calculation_method_and_parameters "SBE 43";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "A detailed and more complete description is available in the cruise report at: https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf. CTD/rosette casts were performed with a package consisting of a 24-place, 10-liter rosette frame (AOMLs yellow frame), a 24-place water sampler/pylon (SBE32) and 24, 10-liter Bullister/Niskin-style bottles. This package was deployed on all stations/casts. Underwater electronic components consisted of a Sea-Bird Electronics (SBE) 9 plus CTD with dual pumps and the following sensors: dual temperature (SBE3), dual conductivity (SBE4), dual dissolved oxygen (SBE43), and a Simrad 807 altimeter. The CTDs supplied a standard Sea-Bird format data stream at a data rate of 24 frames/second. The SBE9plus CTD was connected to the SBE32 24-place pylon providing for single-conductor sea cable operation. Power to the SBE9plus CTD, SBE32 pylon, auxiliary sensors, and altimeter was provided through the sea cable from the SBE11plus deck unit in the computer lab. The raw CTD data and bottle trips acquired by SBE Seasave on the Windows 7 workstation were processed from hex files to cnv files and then into bottle files. Post cruise data processing was completed on a Windows 7 machine running SEABIRD SBE DATA Processing version 7.22.5";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Oxygen Per Unit Mass In Sea Water";
String method_reference "https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf.";
Float32 missing_value -9999.9;
String observation_type "profile";
String parameter_id "195";
String researcher_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String researcher_name "Joe Salisbury";
String sampling_instrument "Sea-Bird SBE-911plus CTD system";
String standard_name "moles_of_oxygen_per_unit_mass_in_sea_water";
String uncertainty "The DO sensors were calibrated to dissolved O2 check samples by matching the up cast bottle trips to CTD bottle files. Post cruise calibration of the sensor determined that there was minimal drift with a slope of 1.0301 ml/L between calibrations. ";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
ph {
Float32 _FillValue -9999.9;
Float32 actual_range 7.600464, 8.121634;
String analyzing_instrument "The pH was measured using the spectrophotometric method on the total hydrogen ion concentration pH scale. The analyzing system consists of an Agilent 8453 UV-visible spectroscopy system, a high precision Kloehn digital pump, a 10-cm light path quartz cell, a thermostated water bath, and a custom-made temperature-control system for spectrophotometer cell.";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Seawater was sampled directly from the Niskin bottle into a narrow neck 125 mL borosilicate glass bottle. After filling the bottle, we let several hundred mL of seawater overflow and then capped the bottle. While awaiting analysis, the samples were stored in the dark. Seawater was analyzed within 2 hours of collection. During analysis, the absorbance of a seawater blank was first measured at three wavelengths (578, 434, and 730 nm). Then the absorbance of the mixture of concentrated purified dye m-cresol purple (30 micro-liter, ~2 mmol/L, MCP) and seawater was measured at the same wavelengths. In addition, a double dye addition experiment was carried out at sea to evaluate the influence on pH due to the addition of dye into seawater.";
String field_replicate_information "73 duplicates were sampled during the cruise.";
String grid_mapping "crs";
String ioos_category "Phytoplankton Species";
String long_name "pH";
String method_reference "Liu, X. W., M. C. Patsavas and R. H. Byrne (2011). Purification and Characterization of meta-Cresol Purple for Spectrophotometric Seawater pH Measurements. Environmental Science & Technology 45(11): 4862-4868. Clayton, T. D. and R. H. Byrne (1993). Spectrophotometric seawater pH measurements - total hydrogen-ion concentration scale calibration of m-cresol purple and at-sea results. Deep-Sea Research Part I 40(10): 2115-2129. Dickson, A. G., C. L. Sabine and J. R. Christian (2007). Guide to Best Practices for Ocean CO2 Measurements.";
Float32 missing_value -9999.9;
String observation_type "Laboratory experiment";
String parameter_id "82";
String ph_scale "total";
String researcher_institution "University of Delaware";
String researcher_name "Wei-Jun Cai";
String sampling_instrument "Niskin bottle and flow through pump";
String standard_name "sea_water_ph_reported_on_total_scale";
String standardization_technique_description "The pH data was guaranteed by purified m-cresol purple which was supplied by Dr. Robert H. Byrne at University of South Florida.";
String temperature_of_measurement "20 C and 25 C. The temperature of measurement for each sample is given under the variable abbreviation PH_TOT_TEMP.";
String uncertainty "< 0.001 pH units";
String unit_id "3";
String units "1";
String variable_type "Manipulation condition";
}
phosphate {
Float32 _FillValue -9999.9;
Float32 actual_range 0.0, 2.49;
String analyzing_instrument "Continuous flow analyzer (CFA) using the standard and analysis protocols for the WOCE hydrographic program as set forth in the manual by L.I. Gordon, et al. (1993).";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Nutrient samples were collected from Niskin bottles, after at least three seawater rinses. Sample analysis typically began within a few hours of sample collection after the samples had warmed to room temperature. Those samples not analyzed within 3 hours were refrigerated for later analysis. Samples were analyzed for phosphate (PO4- 3), nitrate (NO3-), nitrite (NO2-) and orthosilicic acid (H4SiO4). Phosphate was determined by reacting the sample with molybdic acid to form phosphomolybdic acid. This complex was subsequently reduced with hydrazine, and the absorbance of the resulting phosphomolybdous acid was measured at 710 nm.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Phosphate Per Unit Mass In Sea Water";
String method_reference "Armstrong, F.A.J., Stearns, C.R. and Strickland, J.D.H. (1967). The measurement of upwelling and subsequent biological processes by means of the Technicon AutoAnalyzer and associated equipment. Deep-Sea Res. 14:381-389. Gordon, L.I., Jennings Jr., J.C., Ross, A.A. and Krest, J.M. (1993). A suggested protocol for the continuous automated analysis of seawater nutrients (phosphate, nitrate, nitrite and silicic acid) in the WOCE Hydrographic program and the Joint Global Ocean Fluxes Study. WOCE Operations Manual, vol. 3: The Observational Programme, Section 3.2: WOCE Hydrographic Programme, Part 3.1.3: WHP Operations and Methods. WHP Office Report WHPO 91-1; WOCE Report No. 68/91. November 1994, Revision 1, Woods Hole, MA., USA, 52 loose-leaf pages.";
Float32 missing_value -9999.9;
String observation_type "Profile and surface underway";
String parameter_id "131";
String researcher_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String researcher_name "Jia-Zhong Zhang";
String sampling_instrument "Niskin bottle and flow through pump";
String standard_name "phosphate";
String uncertainty "A mixed stock standard consisting of silicic acid, phosphate and nitrate was prepared by dissolving high purity standard materials (KNO3, KH2PO4 and Na2SiF6) in deionized water using a two step dilution for phosphate and nitrate. This standard was stored at room temperature. A nitrite stock standard was prepared dissolving NaNO2 in distilled water, and this standard was stored in a refrigerator on the ship. Working standards were prepared fresh daily by diluting the stock solutions in low nutrient seawater. The mixed standards were verified against commercial standards, and in-lab standards.";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
pressure {
Float32 _FillValue -9999.9;
Float32 actual_range 1.359, 1631.123;
String calculation_method_and_parameters "CTD";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "A detailed and more complete description is available in the cruise report at: https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf. CTD/rosette casts were performed with a package consisting of a 24-place, 10-liter rosette frame (AOMLs yellow frame), a 24-place water sampler/pylon (SBE32) and 24, 10-liter Bullister/Niskin-style bottles. This package was deployed on all stations/casts. Underwater electronic components consisted of a Sea-Bird Electronics (SBE) 9 plus CTD with dual pumps and the following sensors: dual temperature (SBE3), dual conductivity (SBE4), dual dissolved oxygen (SBE43), and a Simrad 807 altimeter. The CTDs supplied a standard Sea-Bird format data stream at a data rate of 24 frames/second. The SBE9plus CTD was connected to the SBE32 24-place pylon providing for single-conductor sea cable operation. Power to the SBE9plus CTD, SBE32 pylon, auxiliary sensors, and altimeter was provided through the sea cable from the SBE11plus deck unit in the computer lab. The raw CTD data and bottle trips acquired by SBE Seasave on the Windows 7 workstation were processed from hex files to cnv files and then into bottle files. Post cruise data processing was completed on a Windows 7 machine running SEABIRD SBE DATA Processing version 7.22.5";
String grid_mapping "crs";
String ioos_category "Pressure";
String long_name "Sea Water Pressure";
String method_reference "https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf.";
Float32 missing_value -9999.9;
String observation_type "profile";
String parameter_id "179";
String researcher_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String researcher_name "Joe Salisbury";
String sampling_instrument "Sea-Bird SBE-911plus CTD system";
String standard_name "sea_water_pressure";
String unit_id "40";
String units "10000.0 Pa";
String variable_type "In-situ observation";
}
profile {
String cf_role "profile_id";
String ioos_category "Unknown";
String long_name "Profile Name";
}
salinity {
Float32 _FillValue -9999.9;
Float32 actual_range 21.5206, 36.911;
String calculation_method_and_parameters "CTD";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "A detailed and more complete description is available in the cruise report at: https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf. CTD/rosette casts were performed with a package consisting of a 24-place, 10-liter rosette frame (AOML’s yellow frame), a 24-place water sampler/pylon (SBE32) and 24, 10-liter Bullister/Niskin-style bottles. This package was deployed on all stations/casts. Underwater electronic components consisted of a Sea-Bird Electronics (SBE) 9 plus CTD with dual pumps and the following sensors: dual temperature (SBE3), dual conductivity (SBE4), dual dissolved oxygen (SBE43), and a Simrad 807 altimeter. The CTDs supplied a standard Sea-Bird format data stream at a data rate of 24 frames/second. The SBE9plus CTD was connected to the SBE32 24-place pylon providing for single-conductor sea cable operation. Power to the SBE9plus CTD, SBE32 pylon, auxiliary sensors, and altimeter was provided through the sea cable from the SBE11plus deck unit in the computer lab. The raw CTD data and bottle trips acquired by SBE Seasave on the Windows 7 workstation were processed from hex files to cnv files and then into bottle files. Post cruise data processing was completed on a Windows 7 machine running SEABIRD SBE DATA Processing version 7.22.5 ";
String grid_mapping "crs";
String ioos_category "Salinity";
String long_name "Salinity";
Float32 missing_value -9999.9;
String observation_type "profile";
String parameter_id "50";
String researcher_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String researcher_name "Joe Salisbury";
String sampling_instrument "Sea-Bird SBE-911plus CTD system";
String standard_name "sea_water_practical_salinity";
String uncertainty "Conductivity sensor calibration coefficients derived from the pre-cruise calibrations were applied to raw primary and secondary conductivities. Comparisons between the primary and secondary sensors and between each of the sensors to check sample conductivities. Post cruise calibration of the primary sensor determined the sensor drift to be 0.0008 PSU/month.";
String unit_id "4";
String units "1e-3";
String variable_type "In-situ observation";
}
silicate {
Float32 _FillValue -9999.9;
Float32 actual_range -0.7, 41.4;
String analyzing_instrument "Continuous flow analyzer (CFA) using the standard and analysis protocols for the WOCE hydrographic program as set forth in the manual by L.I. Gordon, et al. (1993).";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "Nutrient samples were collected from Niskin bottles, after at least three seawater rinses. Sample analysis typically began within a few hours of sample collection after the samples had warmed to room temperature. Those samples not analyzed within 3 hours were refrigerated for later analysis. Samples were analyzed for phosphate (PO4- 3), nitrate (NO3-), nitrite (NO2-) and orthosilicic acid (H4SiO4). Silicic acid was analyzed using a modification of Armstrong et al. (1967). The sample is reacted with ammonium molybdate in an acidic solution to form molybdosilicic acid. The molybdosilicic acid was then reduced with ascorbic acid to form molybdenum blue. The absorbance of the molybdenum blue was measured at 660 nm.";
String grid_mapping "crs";
String ioos_category "Unknown";
String long_name "Moles Of Silicate Per Unit Mass In Sea Water";
String method_reference "Armstrong, F.A.J., Stearns, C.R. and Strickland, J.D.H. (1967). The measurement of upwelling and subsequent biological processes by means of the Technicon AutoAnalyzer and associated equipment. Deep-Sea Res. 14:381-389. Gordon, L.I., Jennings Jr., J.C., Ross, A.A. and Krest, J.M. (1993). A suggested protocol for the continuous automated analysis of seawater nutrients (phosphate, nitrate, nitrite and silicic acid) in the WOCE Hydrographic program and the Joint Global Ocean Fluxes Study. WOCE Operations Manual, vol. 3: The Observational Programme, Section 3.2: WOCE Hydrographic Programme, Part 3.1.3: WHP Operations and Methods. WHP Office Report WHPO 91-1; WOCE Report No. 68/91. November 1994, Revision 1, Woods Hole, MA., USA, 52 loose-leaf pages.";
Float32 missing_value -9999.9;
String observation_type "Profile and surface underway";
String parameter_id "133";
String researcher_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String researcher_name "Jia-Zhong Zhang";
String standard_name "silicate";
String uncertainty "A mixed stock standard consisting of silicic acid, phosphate and nitrate was prepared by dissolving high purity standard materials (KNO3, KH2PO4 and Na2SiF6) in deionized water using a two step dilution for phosphate and nitrate. This standard was stored at room temperature. A nitrite stock standard was prepared dissolving NaNO2 in distilled water, and this standard was stored in a refrigerator on the ship. Working standards were prepared fresh daily by diluting the stock solutions in low nutrient seawater. The mixed standards were verified against commercial standards, and in-lab standards.";
String unit_id "57";
String units "micromol.kg-1";
String variable_type "In-situ observation";
}
temperature {
Float32 _FillValue -9999.9;
Float32 actual_range 0.9373, 30.5234;
String calculation_method_and_parameters "CTD";
String cell_methods "time: point lon: point lat: point z: point";
String coordinates "time latitude longitude z";
String coverage_content_type "physicalMeasurement";
String data_quality_flag_description "WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value, 5 = value not reported, 6 = mean of replicate measurements, 9 = sample not drawn.";
String detailed_sampling_and_analyzing_information "A detailed and more complete description is available in the cruise report at: https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf. CTD/rosette casts were performed with a package consisting of a 24-place, 10-liter rosette frame (AOML’s yellow frame), a 24-place water sampler/pylon (SBE32) and 24, 10-liter Bullister/Niskin-style bottles. This package was deployed on all stations/casts. Underwater electronic components consisted of a Sea-Bird Electronics (SBE) 9 plus CTD with dual pumps and the following sensors: dual temperature (SBE3), dual conductivity (SBE4), dual dissolved oxygen (SBE43), and a Simrad 807 altimeter. The CTDs supplied a standard Sea-Bird format data stream at a data rate of 24 frames/second. The SBE9plus CTD was connected to the SBE32 24-place pylon providing for single-conductor sea cable operation. Power to the SBE9plus CTD, SBE32 pylon, auxiliary sensors, and altimeter was provided through the sea cable from the SBE11plus deck unit in the computer lab. The raw CTD data and bottle trips acquired by SBE Seasave on the Windows 7 workstation were processed from hex files to cnv files and then into bottle files. Post cruise data processing was completed on a Windows 7 machine running SEABIRD SBE DATA Processing version 7.22.5 ";
String grid_mapping "crs";
String ioos_category "Temperature";
String long_name "Sea Water Temperature";
Float32 missing_value -9999.9;
String observation_type "profile";
String parameter_id "41";
String researcher_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String researcher_name "Joe Salisbury";
String sampling_instrument "Sea-Bird SBE-911plus CTD system";
String standard_name "sea_water_temperature";
String uncertainty "Conductivity sensor calibration coefficients derived from the pre-cruise calibrations were applied to raw primary and secondary conductivities. Comparisons between the primary and secondary sensors and between each of the sensors to check sample conductivities. Post cruise calibration of the primary sensor determined the sensor drift to be 0.0008 PSU/month.";
String unit_id "8";
String units "degree_Celsius";
String variable_type "In-situ observation";
}
time {
String _CoordinateAxisType "Time";
Float64 actual_range 1.434765195e+9, 1.437669793e+9;
String axis "T";
String calendar "standard";
String ioos_category "Time";
String long_name "Sample Time";
String standard_name "time";
String time_origin "01-JAN-1970 00:00:00";
String units "seconds since 1970-01-01T00:00:00Z";
}
z {
String _CoordinateAxisType "Height";
Float32 _FillValue -9999.9;
Float32 actual_range 1.757, 1613.541;
String axis "Z";
String calculation_method_and_parameters "CTD";
String cell_methods "time: point lon: point lat: point z: point";
String comment "depth was calculated from pressure using Sea-Bird Electronics document AN69, http://www.seabird.com/document/an69-conversion-pressure-depth";
String coverage_content_type "physicalMeasurement";
String detailed_sampling_and_analyzing_information "A detailed and more complete description is available in the cruise report at: https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf. CTD/rosette casts were performed with a package consisting of a 24-place, 10-liter rosette frame (AOMLs yellow frame), a 24-place water sampler/pylon (SBE32) and 24, 10-liter Bullister/Niskin-style bottles. This package was deployed on all stations/casts. Underwater electronic components consisted of a Sea-Bird Electronics (SBE) 9 plus CTD with dual pumps and the following sensors: dual temperature (SBE3), dual conductivity (SBE4), dual dissolved oxygen (SBE43), and a Simrad 807 altimeter. The CTDs supplied a standard Sea-Bird format data stream at a data rate of 24 frames/second. The SBE9plus CTD was connected to the SBE32 24-place pylon providing for single-conductor sea cable operation. Power to the SBE9plus CTD, SBE32 pylon, auxiliary sensors, and altimeter was provided through the sea cable from the SBE11plus deck unit in the computer lab. The raw CTD data and bottle trips acquired by SBE Seasave on the Windows 7 workstation were processed from hex files to cnv files and then into bottle files. Post cruise data processing was completed on a Windows 7 machine running SEABIRD SBE DATA Processing version 7.22.5";
String grid_mapping "crs";
String ioos_category "Location";
String long_name "Depth";
String method_reference "https://www.aoml.noaa.gov/ocd/gcc/ECOA1/Cruise_Report.pdf.";
Float32 missing_value -9999.9;
String observation_type "profile";
String positive "down";
String researcher_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String researcher_name "Joe Salisbury";
String sampling_instrument "Sea-Bird SBE-911plus CTD system";
String standard_name "depth";
String units "m";
Float32 valid_max 1620.0;
Float32 valid_min 0.0;
String variable_type "In-situ observation";
}
}
NC_GLOBAL {
String abstract "The East Coast Ocean Acidification (ECOA) Cruise on board the R/V Gordan Gunter from Newport, took place in the Gulf of Maine and then along the East US coast to Miami. The effort was in support of the coastal monitoring and research objectives of the NOAA Ocean Acidification Program (OAP). The cruise was designed to obtain a snapshot of key carbon, physical, and biogeochemical parameters as they relate to ocean acidification (OA) in the coastal realm. The cruise included a series of 11 transects approximately orthogonal to the Gulf of Maine and Atlantic coasts and a comprehensive set of underway measurements along the entire transect.";
String abstract_ncei "This archival package contains dissolved inorganic carbon, total alkalinity, pH, nutrients and other variables collected from profile and discrete sample observations during the East Coast Ocean Acidification (GU-15-04 ECOA1). The East Coast Ocean Acidification (ECOA) Cruise on board NOAA Ship Gordon Gunter from Newport, took place in the Gulf of Maine and then along the East US coast to Miami. The effort was in support of the coastal monitoring and research objectives of the NOAA Ocean Acidification Program (OAP). The cruise was designed to obtain a snapshot of key carbon, physical, and biogeochemical parameters as they relate to ocean acidification (OA) in the coastal realm. The cruise included a series of 11 transects approximately orthogonal to the Gulf of Maine and Atlantic coasts and a comprehensive set of underway measurements along the entire transect.";
String cdm_altitude_proxy "z";
String cdm_data_type "Profile";
String cdm_profile_variables "profile";
String citation "Salisbury, J. 2016. ECOA cruise station discrete data. National Oceanographic Data Center.";
String contributor_name_10_address "4301 Rickenbacker Causeway, Miami, FL 33149, USA";
String contributor_name_10_email "Jia-Zhong.Zhang@noaa.gov";
String contributor_name_10_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String contributor_name_10_name "Jia-Zhong Zhang";
String contributor_name_10_phone "305-361-4512";
String contributor_name_10_role "PI";
String contributor_name_11_address "104 CEOAS Admin Bldg., Corvallis, OR 97331";
String contributor_name_11_email "ljuranek@coas.oregonstate.edu";
String contributor_name_11_institution "College of Earth, Ocean, and Atmospheric Sciences, Oregon State University";
String contributor_name_11_name "Lauren Jurank";
String contributor_name_11_phone "541-737-2368";
String contributor_name_11_role "PI";
String contributor_name_1_address "8 College Road, Durham, NH 03824, USA";
String contributor_name_1_email "Joe.Salisbury@unh.edu";
String contributor_name_1_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String contributor_name_1_name "Joe Salisbury";
String contributor_name_1_phone "603-862-0849";
String contributor_name_2_address "014 Lammot DuPont Lab, Newark, DE 19716";
String contributor_name_2_email "wcai@udel.edu";
String contributor_name_2_institution "College of Earth, Ocean, and the Environment, University of Delaware";
String contributor_name_2_name "Wei-Jun Cai";
String contributor_name_2_phone "302-831-2839";
String contributor_name_3_address "4301 Rickenbacker Causeway, Miami, FL 33149, USA";
String contributor_name_3_email "Rik.Wanninkhof@noaa.gov";
String contributor_name_3_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String contributor_name_3_name "Rik Wanninkhof";
String contributor_name_3_phone "305-361-4379";
String contributor_name_4_address "4301 Rickenbacker Causeway, Miami, FL 33149, USA";
String contributor_name_4_email "Leticia.Barbero@noaa.gov";
String contributor_name_4_institution "Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration";
String contributor_name_4_name "Leticia Barbero";
String contributor_name_4_phone "305-361-4453";
String contributor_name_4_role "PI";
String contributor_name_5_address "8 College Road, Durham NH 03824";
String contributor_name_5_email "shawn.shellito@unh.edu";
String contributor_name_5_institution "University of New Hampshire";
String contributor_name_5_name "Shawn Shellito";
String contributor_name_5_phone "603-862-2999";
String contributor_name_5_role "PI";
String contributor_name_6_address "8 College Road, Durham NH 03824";
String contributor_name_6_email "bror.jonsson@unh.edu";
String contributor_name_6_institution "University of New Hampshire";
String contributor_name_6_name "Bror Jonsson";
String contributor_name_6_phone "603-862-3421";
String contributor_name_6_role "PI";
String contributor_name_7_address "4600 Rickenbacker Causeway, Miami, FL 33149";
String contributor_name_7_email "clangdon@rsmas.miami.edu";
String contributor_name_7_institution "University of Miami";
String contributor_name_7_name "Chris Langdon";
String contributor_name_7_phone "305-421-4614";
String contributor_name_7_role "PI";
String contributor_name_8_address "Mail Code 616.1, Greenbelt, MD 20771";
String contributor_name_8_email "antonio.mannino-1@nasa.gov";
String contributor_name_8_institution "NASA Goddard Space Flight Center";
String contributor_name_8_name "Antonio Mannino";
String contributor_name_8_phone "301-286-0182";
String contributor_name_8_role "PI";
String contributor_name_9_address "435 Oceanography & Physics Bldg, Norfolk VA 23529";
String contributor_name_9_email "mmulholl@odu.edu";
String contributor_name_9_institution "Old Dominion University";
String contributor_name_9_name "Margaret Mulholland";
String contributor_name_9_phone "757-683-3972";
String contributor_name_9_role "PI";
String Conventions "CF-1.6, ACDD-1.3";
String creator_email "luc@axiomdatascience.com, rob@axiomdatascience.com";
String creator_name "Axiom Data Science";
String creator_url "http://www.axiomdatascience.com/";
String cruise_id "GU-15-04 ECOA1";
String data_submitter_address "8 College Road, Durham, NH 03824, USA";
String data_submitter_email "shawn.shellito@unh.edu";
String data_submitter_institution "Ocean Processes Analysis Laboratory, University of New Hampshire";
String data_submitter_name "Shawn Shellito";
String data_submitter_phone "603-862-0849";
String date_created "2017-11-07T19:53:20Z";
String date_metadata_modified "2017-11-07T19:53:20Z";
String date_submitted "2017-07-10T00:00:00.000-08:00";
Float64 Easternmost_Easting -61.72616;
String expocode "33GG20150619";
String featureType "Profile";
String funding_agency_name "NOAA's Ocean Acidification Program";
String funding_project_id "NA11NOS0120034";
String funding_project_title "ECOA Cruise";
String geospatial_bounds "POLYGON ((-79.18116760253906 26.98217010498047, -79.49810028076172 26.98287010192871, -79.86715698242188 26.99032020568848, -80.00131988525391 27.00016021728516, -80.57916259765625 28.7544994354248, -80.97350311279297 31.47359085083008, -75.14631652832031 38.91682052612305, -73.87580108642578 40.37451171875, -69.93182373046875 43.50899887084961, -66.64700317382812 44.87250137329102, -66.36598205566406 44.94449996948242, -63.45800018310547 44.39865875244141, -62.87366104125977 43.88150024414062, -61.87815856933594 42.99681854248047, -61.82500076293945 42.93865966796875, -61.72615814208984 42.83000183105469, -79.18116760253906 26.98217010498047))";
String geospatial_bounds_crs "EPSG:4326";
Float64 geospatial_lat_max 44.9445;
Float64 geospatial_lat_min 26.98217;
String geospatial_lat_units "degrees_north";
Float64 geospatial_lon_max -61.72616;
Float64 geospatial_lon_min -80.9735;
String geospatial_lon_units "degrees_east";
String geospatial_vertical_max "1613.54";
String geospatial_vertical_min "1.35";
String geospatial_vertical_positive "down";
String geospatial_vertical_reference "mean_sea_level";
String geospatial_vertical_units "meters";
String history
"Mon Feb 5 10:10:03 2018: ncks -v pressure,temperature,profile,salinity,ph,chl_a,silicate,nitrite,nitrate,nitrate_nitrite,phosphate,nitrogen,cdom,oxygen_concentration GU_15_04_ECOA1_1434765195_1437670876.full.nc GU_15_04_ECOA1_1434765195_1437670876.nc
NetCDF generated by Axiom from NCEI archived files
2025-07-08T10:50:07Z https://files.stage.platforms.axds.co/axiom/netcdf_harvest/socan/GU_15_04_ECOA1_1434765195_1437670876/processed.nc
2025-07-08T10:50:07Z http://erddap.secoora.org/tabledap/axiom-netcdf-harvest-socan-GU-15-04-ECOA1-1434765195-1437670876.das";
String id "GU_15_04_ECOA1";
String infoUrl "https://portal.axds.co/?portal_id=47#platform/4b2c7f1f-439f-56d2-b35f-274be6dfb983/v2";
String institution "NOAA OAP";
String keywords "ALKALINITY, CHLOROPHYLL A, Chromophoric Dissolved Organic Matter (CDOM), DISSOLVED INORGANIC CARBON (DIC), DISSOLVED ORGANIC CARBON, DISSOLVED OXYGEN, NITRATE, nitrate + nitrite content (concentration), NITRITE, NITROGEN - PARTICULATE, OCEAN CHEMISTRY, PARTICULATE ORGANIC CARBON, PH, PHOSPHATE, SALINITY, SILICATE, WATER TEMPERATURE";
String keywords_vocabulary "GCMD Earth Science Keywords. Version 5.3.3";
String license
"The data may be used and redistributed for free but is not intended
for legal use, since it may contain inaccuracies. Neither the data
Contributor, ERD, NOAA, nor the United States Government, nor any
of their employees or contractors, makes any warranty, express or
implied, including warranties of merchantability and fitness for a
particular purpose, or assumes any legal liability for the accuracy,
completeness, or usefulness, of this information.";
String Metadata_Conventions "Unidata Dataset Discovery v1.0";
String metadata_link "https://www.nodc.noaa.gov/cgi-bin/OAS/prd/accession/159428";
String naming_authority "gov.noaa.ncei";
String ncei_accession_number "0159428";
String ncei_template_version "NCEI_NetCDF_Profile_Incomplete_Template_v2.0";
String NCO "4.4.2";
Float64 Northernmost_Northing 44.9445;
String packrat_source "axiom.netcdf_harvest.netcdf_harvest";
String packrat_source_id "socan/GU_15_04_ECOA1_1434765195_1437670876";
String packrat_uuid "4b2c7f1f-439f-56d2-b35f-274be6dfb983";
String platform "RV Gordon Gunter";
String platform_category "cruise";
String platform_country "USA";
String platform_ircs "WTEO";
String platform_ncei "33GG";
String platform_owner "NOAA";
String platform_type "Research Vessel";
String platform_wod "7607";
String project "ECOA1";
String references "Salisbury, J. 2016. ECOA Report.";
String sea_name "East Coast - US/Canada";
String source "NOAA OAP";
String sourceUrl "https://files.stage.platforms.axds.co/axiom/netcdf_harvest/socan/GU_15_04_ECOA1_1434765195_1437670876/processed.nc";
Float64 Southernmost_Northing 26.98217;
String standard_name_vocabulary "NetCDF Climate and Forecast (CF) Metadata Convention Standard Name Table v46";
String subsetVariables "latitude, longitude, profile, time";
String summary "To measure key carbon, physical and biogeochemical parameters in coastal waters of the Gulf of Maine and eastern coast of the US in relation to Ocean Acidification.";
String supplemental_information "https://www.aoml.noaa.gov/ocd/gcc/ECOA1";
Float64 time_coverage_duration 2.905681e+9;
String time_coverage_end "2015-07-23T16:43:13Z";
String time_coverage_start "2015-06-20T01:53:15Z";
String title "(SECOORA) Glider - ECOA1 - ECOA1 Discrete Sampling: Dissolved inorganic carbon, total alkalinity, pH, nutrients and other variables collected from profile and discrete sample observations using CTD, Niskin bottle, and other instruments from NOAA Ship Gordon Gunter off the U.S. East Coast during the East Coast Ocean Acidification (GU-15-04 ECOA1) from 2015-06-20 to 2015-07-23 (NCEI Accession 0159428).";
String urn "urn:ioos:station:gov.noaa.ncei:GU_15_04_ECOA1";
String vessel_name "RV Gordon Gunter";
Float64 Westernmost_Easting -80.9735;
}
}
Data Access Protocol (DAP) and its
selection constraints.
The URL specifies what you want: the dataset, a description of the graph or the subset of the data, and the file type for the response.
Tabledap request URLs must be in the form
https://coastwatch.pfeg.noaa.gov/erddap/tabledap/datasetID.fileType{?query}
For example,
https://coastwatch.pfeg.noaa.gov/erddap/tabledap/pmelTaoDySst.htmlTable?longitude,latitude,time,station,wmo_platform_code,T_25&time>=2015-05-23T12:00:00Z&time<=2015-05-31T12:00:00Z
Thus, the query is often a comma-separated list of desired variable names,
followed by a collection of
constraints (e.g., variable<value),
each preceded by '&' (which is interpreted as "AND").
For details, see the tabledap Documentation.