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Namespace Prefixes

PrefixIRI
n19http://vocab.nerc.ac.uk/collection/P64/current/G963/
n9http://vocab.nerc.ac.uk/collection/P07/current/CFSN0464/3/
dctermshttp://purl.org/dc/terms/
n15http://vocab.nerc.ac.uk/collection/P07/current/DHTXFX9K/
dchttp://purl.org/dc/elements/1.1/
skoshttp://www.w3.org/2004/02/skos/core#
n2http://vocab.nerc.ac.uk/standard_name/ocean_integral_of_sea_water_temperature_wrt_depth/
voidhttp://rdfs.org/ns/void#
n14http://vocab.nerc.ac.uk/collection/P07/current/9W3159BW/
n16http://vocab.nerc.ac.uk/collection/P02/current/TEMP/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n6http://vocab.nerc.ac.uk/collection/P06/current/KMTX/
owlhttp://www.w3.org/2002/07/owl#
n4http://vocab.nerc.ac.uk/.well-known/
xsdhhttp://www.w3.org/2001/XMLSchema#
n10http://vocab.nerc.ac.uk/collection/P07/current/CFSN0464/1/
n18http://vocab.nerc.ac.uk/collection/P04/current/G963/
n8http://purl.org/pav/
n13http://vocab.nerc.ac.uk/collection/P07/current/CFSN0464/2/
n12http://mmisw.org/ont/cf/parameter/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
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owl:sameAs
n12:ocean_integral_of_sea_water_temperature_wrt_depth n14: n2: n15:
skos:broader
n16: n18: n19:
skos:prefLabel
ocean_integral_of_sea_water_temperature_wrt_depth
dcterms:identifier
SDN:P07::CFSN0464
dc:identifier
SDN:P07::CFSN0464
dcterms:date
2017-11-28 06:51:06.0
skos:definition
"integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to. Depth is the vertical distance below the surface. Sea water temperature is the in situ temperature of the sea water. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard "scales". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990.
skos:notation
SDN:P07::CFSN0464
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owl:deprecated
true
skos:note
deprecated
void:inDataset
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n6:
n8:authoredOn
2017-11-28 06:51:06.0
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n9:
n8:hasVersion
n10: n13:
n8:version
3