{"@context":{"content":"http://purl.org/rss/1.0/modules/content/","dc":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","og":"http://ogp.me/ns#","rdfs":"http://www.w3.org/2000/01/rdf-schema#","sioc":"http://rdfs.org/sioc/ns#","sioct":"http://rdfs.org/sioc/types#","skos":"http://www.w3.org/2004/02/skos/core#","xsd":"http://www.w3.org/2001/XMLSchema#","owl":"http://www.w3.org/2002/07/owl#","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","rss":"http://purl.org/rss/1.0/","site":"https://osprey.bco-dmo.org/ns#","odo":"http://ocean-data.org/schema/","emo":"http://ocean-data.org/schema/entity-matching#","bibo":"http://purl.org/ontology/bibo/","crypto":"http://id.loc.gov/vocabulary/preservation/cryptographicHashFunctions/","bcodmo":"http://lod.bco-dmo.org/id/","tw":"http://tw.rpi.edu/schema/","dcat":"http://www.w3.org/ns/dcat#","time":"http://www.w3.org/2006/time#","geo":"http://www.w3.org/2003/01/geo/wgs84_pos#","geosparql":"http://www.opengis.net/ont/geosparql#","sf":"http://www.opengis.net/ont/sf#","void":"http://rdfs.org/ns/void#","sd":"http://www.w3.org/ns/sparql-service-description#","dctype":"http://purl.org/dc/dcmitype/","prov":"http://www.w3.org/ns/prov#","schema":"http://schema.org/","geolink":"http://schema.geolink.org/1.0/base/main#","spdx":"http://spdx.org/rdf/terms#","bcodmo_vocab":"http://schema.bco-dmo.org/"},"@id":"http://lod.bco-dmo.org/id/dataset/728371#graph","@graph":[{"http://lod.bco-dmo.org/id/dataset/728371":{"@id":"http://lod.bco-dmo.org/id/dataset/728371","@type":["http://ocean-data.org/schema/DeploymentDatasetCollection","http://www.w3.org/ns/dcat#Dataset","http://ocean-data.org/schema/Dataset"],"http://ocean-data.org/schema/hasAcquisitionDescription":[{"@value":"<div><p>Multiple deployments of two Sea-Bird Scientific Navis BGCi floats (numbers F033 and F034) equipped with CTDs, transmissometers, O2 optodes, backscattering (700 nm), fluorescence (chlorophyll, colored dissolved organic matter), and tilt sensors were conducted between July 2013 and November 2014 in conjunction with Bermuda Atlantic Time-series Study cruises. Short-term deployments (1.5 \u2013 3 days) followed by recovery of the floats were conducted during four monthly BATS cruises in July \u2013 October 2013 and one cruise in March 2014. Both floats were deployed during the July and August 2013 cruises and float F034 was deployed for the remaining cruises. Each float collected one profile per cruise with the exception of the August 2013 cruise, during which the two floats together collected 13 profiles. During short-term deployments, floats first completed an initial descent and ascent without parking, then completed 1 or 2 more profile cycles with different, consecutive target depths. Following the initial descent/ascent described above, the short-term profile cycles were structured as described below for long-term deployments. In addition to the short-term cruise deployments, F033 profiled continuously from October 2013 until early April 2014, yielding 77 profiles, and F034 profiled continuously from March 2014 until late November 2014, yielding 139 profiles. During these long-term deployments, a typical cycle consisted of 1) the descent to the target park depth, 2) a park phase at the target depth lasting 1.5 \u2013 2.5 days during which measurements are made every 15 minutes, 3) a descent to 1000 dbar, 4) an ascent to the surface during which measurements are made, and 5) a surface telemetry phase, during which a GPS fix is obtained, data are uploaded via Iridium, and instructions for the next cycle are downloaded. During long-term deployments, floats cycled through park phases at 150/200, 300, 500, and 1000 dbar every 7 days, spending 2.5 days at 1000 dbar and 1.5 days at the shallower depths. The sequence of park phase depth at the three shallowest depths was varied between each 7-day cycle over a 21-day period to avoid aliasing in particle flux profiles.</p>\n<p>Refer to <a href=\"http://www.bco-dmo.org/project/2124\">http://www.bco-dmo.org/project/2124</a> or <a href=\"http://bats.bios.edu/\">http://bats.bios.edu</a> for a description of BATS bottle sample acquisition.</p></div>","@type":"rdf:HTML"}],"http://ocean-data.org/schema/hasBriefDescription":[{"@value":"Factory and field calibration data for float oxygen, beam transmission, backscatter, chlorophyll fluorescence and CDOM sensors from the Sargasso Sea from 2013-2014","@language":"en-US"}],"http://purl.org/dc/terms/description":[{"@value":"<div><p>Factory and field calibration data for float oxygen, beam transmission, backscatter, chlorophyll fluorescence and CDOM sensors from the Sargasso Sea from 2013-2014.</p></div>","@type":"rdf:HTML"}],"http://www.w3.org/2000/01/rdf-schema#label":[{"@value":"Sensor calibration data","@type":"xsd:string"}],"http://ocean-data.org/schema/hasProcessingDescription":[{"@value":"<div><p><span style=\"font-size:14px\">The following are factory and field determined calibration coefficients for float oxygen, beam transmission, chlorophyll fluorescence, backscatter, and CDOM sensors. Calibrated float data are presented in the \u2018Profile data\u2019 (<a href=\"https://www.bco-dmo.org/dataset/728347\" style=\"color: purple;\">https://www.bco-dmo.org/dataset/728347</a>) and \u2018Park phase data\u2019 (<a href=\"https://www.bco-dmo.org/dataset/728335\" style=\"color: purple;\">https://www.bco-dmo.org/dataset/728335</a>) datasets\u2019. Float oxygen, chlorophyll fluorescence, and backscatter data were additionally calibrated to BATS bottle samples from concurrent BATS cruises. When possible, each float sample collected in profile mode was matched to the BATS bottle sample nearest in potential density that was collected within a 10-km radius and \u00b115-m depth window of the float location within 1 d of the float sampling time. The BATS bottle data used for float calibration are provided for reference through the \u2018Get Data\u2019 link at the top of this page. Original BATS bottle data are available at <a href=\"http://www.bco-dmo.org/project/2124\" style=\"color: purple;\">http://www.bco-dmo.org/project/2124</a> or\u00a0<span style=\"font-family:calibri,sans-serif\"><a href=\"http://bats.bios.edu/\" style=\"color: purple;\">http://bats.bios.edu</a>.</span></span></p>\n<p><img alt=\"\" src=\"/objectserver/07a9fe9195a7cff1800880ee653b6f0d/Table1.png?url=http%3A%2F%2Fdmoserv3.bco-dmo.org%2Fdata_docs%2FRapAutParticleFlux%2FTable1.png&f=3333333337383833383736393139656133613864636266336633333239396533687474703a2f2f646d6f73657276332e62636f2d646d6f2e6f72672f646174615f646f63732f5261704175745061727469636c65466c75782f5461626c65312e706e67\" style=\"height:445px; width:373px\" /></p>\n<p><img alt=\"\" src=\"https://datadocs.bco-dmo.org/docs/305/RapAutParticleFlux/data_docs/728371/Table_3.png\" style=\"height:445px; width:498px\" /></p>\n<p><img alt=\"\" src=\"https://datadocs.bco-dmo.org/docs/305/RapAutParticleFlux/data_docs/728371/Table_6.png\" style=\"height:445px; width:477px\" /></p>\n<p><strong>BCO-DMO Data Processing Description:</strong></p>\n<p>-Reformatted column names to comply with BCO-DMO standards.<br />\n-Data were originally organized into multiples files and have been consolidated for display here.</p>\n<p>\u00a0</p></div>","@type":"rdf:HTML"}],"http://purl.org/dc/terms/identifier":[{"@value":"728371","@type":"xsd:int"}],"http://purl.org/dc/terms/title":[{"@value":"Sensor calibration data"}],"http://purl.org/dc/terms/date":[{"@value":"2018-02-26T15:24:44-05:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/created":[{"@value":"2018-02-26T15:24:44-05:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/modified":[{"@value":"2023-07-07T16:10:26-04:00","@type":"xsd:dateTime"}],"http://rdfs.org/ns/void#inDataset":[{"@id":"http://www.bco-dmo.org/"}],"http://ocean-data.org/schema/namedGraph":[{"@value":"urn:bcodmo:dataset:728371","@type":"xsd:token"}],"http://ocean-data.org/schema/osprey_page":[{"@id":"https://osprey.bco-dmo.org/dataset/728371"}],"http://ocean-data.org/schema/identifier":[{"@id":"urn:bcodmo:osprey:v2:node:identifier:728371"}],"http://ocean-data.org/schema/browseGraphic":[{"@value":"https://datadocs.bco-dmo.org/docs/305/RapAutParticleFlux/data_docs/browse_graphic.png","@type":"xsd:anyURI"}],"http://ocean-data.org/schema/datasetTitle":[{"@value":"Factory and field calibration data for float oxygen, beam transmission, backscatter, chlorophyll fluorescence and CDOM sensors from the Sargasso Sea from 2013-2014.","@language":"en-US"}],"http://ocean-data.org/schema/abstract":[{"@value":"Optical proxy measurements of sinking particle flux and water-column bio-optical profiles were obtained from profiling floats in the Sargasso Sea to expand the number of particle flux observations in the critical and under-sampled \u201ctwilight zone\u201d. Factory and field calibration data for dissolved oxygen, beam transmission, optical backscatter, chlorophyll fluorescence and colored dissolved organic matter sensors are provided. Float oxygen, chlorophyll fluorescence, and backscatter sensors were additionally cross-calibrated to bottle samples for oxygen, HPLC chlorophyll, and particulate organic carbon collected during concurrent Bermuda Atlantic Time-series Study (BATS) cruises prior to months-long deployment of the floats in the Sargasso Sea.","@language":"en-US"}],"http://purl.org/dc/terms/rights":[{"@id":"https://creativecommons.org/licenses/by/4.0/"}],"http://ocean-data.org/schema/deprecated":[{"@value":"false","@type":"xsd:boolean"}],"http://ocean-data.org/schema/temporalExtent":[{"@id":"urn:bcodmo:dataset:728371:temporalExtent"}],"http://ocean-data.org/schema/spatialCoverage":[{"@id":"urn:bcodmo:dataset:728371:spatialCoverage"}],"http://purl.org/dc/terms/bibliographicCitation":[{"@value":"Estapa, M., Buesseler, K. (2018) Factory and field calibration data for float oxygen, beam transmission, backscatter, chlorophyll fluorescence and CDOM sensors from the Sargasso Sea from 2013-2014. Biological and Chemical Oceanography Data Management Office (BCO-DMO). 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