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BCO-DMO ERDDAP
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Dataset Title: | [Turbulence microstructure profiles] - Turbulence microstructure profiles collected during R/V Hugh R. Sharp cruise HRS2204 from Apr to May 2022 (Collaborative Research: The importance of particle disaggregation on biogeochemical flux predictions) ![]() ![]() |
Institution: | BCO-DMO (Dataset ID: bcodmo_dataset_945981_v1) |
Information: | Summary ![]() ![]() ![]() |
Attributes { s { Deployment_ID { String long_name "Deployment_id"; String units "unitless"; } Station { Int32 actual_range 1, 8; String long_name "Station"; String units "unitless"; } Station_Deployment { Int32 actual_range 1, 3; String long_name "Station_deployment"; String units "unitless"; } Station_Deployment_Profile { Int32 actual_range 1, 3; String long_name "Station_deployment_profile"; String units "unitless"; } Cruise_Deployment { String long_name "Cruise_deployment"; String units "unitless"; } time { String _CoordinateAxisType "Time"; Float64 actual_range 1.65074316e+9, 1.6514472e+9; String axis "T"; String ioos_category "Time"; String long_name "Iso_datetime_utc"; String standard_name "time"; String time_origin "01-JAN-1970 00:00:00"; String units "seconds since 1970-01-01T00:00:00Z"; } latitude { String _CoordinateAxisType "Lat"; Float32 actual_range 39.457, 41.764; String axis "Y"; String ioos_category "Location"; String long_name "Latitude"; String standard_name "latitude"; String units "degrees_north"; } longitude { String _CoordinateAxisType "Lon"; Float32 actual_range -72.266, -67.399; String axis "X"; String ioos_category "Location"; String long_name "Longitude"; String standard_name "longitude"; String units "degrees_east"; } t_rel { Float32 actual_range 139.5145, 3614.921; String long_name "T_rel"; String units "seconds"; } p { Float32 actual_range 8.6121, 357.2398; String long_name "P"; String units "dbar"; } T { Float32 actual_range 6.314, 15.079; String long_name "T"; String units "degrees Celsius"; } e { Float32 actual_range 2.127e-10, 6.612e-5; String long_name "E"; String units "watts per kilogram (W/kg)"; } } NC_GLOBAL { String cdm_data_type "Other"; String Conventions "COARDS, CF-1.6, ACDD-1.3"; String creator_email "info@bco-dmo.org"; String creator_name "BCO-DMO"; String creator_url "https://www.bco-dmo.org/"; String defaultDataQuery "&time<now"; String doi "10.26008/1912/bco-dmo.945981.1"; Float64 Easternmost_Easting -67.399; Float64 geospatial_lat_max 41.764; Float64 geospatial_lat_min 39.457; String geospatial_lat_units "degrees_north"; Float64 geospatial_lon_max -67.399; Float64 geospatial_lon_min -72.266; String geospatial_lon_units "degrees_east"; String history "2025-02-28T16:53:49Z (local files) 2025-02-28T16:53:49Z https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_945981_v1.html"; String infoUrl "https://www.bco-dmo.org/dataset/945981"; String institution "BCO-DMO"; 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."; Float64 Northernmost_Northing 41.764; String sourceUrl "(local files)"; Float64 Southernmost_Northing 39.457; String summary "These data include profiles of turbulence dissipation rate obtained from a Rockland Scientific VMP-250 deployed during a cruise on the Northeast Continental Shelf to study particle disaggregation. One cruise was completed aboard the R/V Hugh R. Sharp from 2022-04-21 through 2022-05-02 (HRS22-04), which visited a variety of stations and hydrodynamic environments associated with the Northeast Continental Shelf of the United States. Cruise stations where dissipation rate profiles were obtained ranged from Georges Bank and the Great South Channel near the Gulf of Maine, and Hudson Canyon near New York. These data were collected as part of a study to clarify the importance of hydrodynamic forces on the cohesion, aggregation, and breakup of marine particles. These data were collected by Dr. Matthew Rau (chief-sci) of the George Washington University."; String time_coverage_end "2022-05-01T23:20:00Z"; String time_coverage_start "2022-04-23T19:46:00Z"; String title "[Turbulence microstructure profiles] - Turbulence microstructure profiles collected during R/V Hugh R. Sharp cruise HRS2204 from Apr to May 2022 (Collaborative Research: The importance of particle disaggregation on biogeochemical flux predictions)"; Float64 Westernmost_Easting -72.266; } }
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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.