This HTML5 document contains 24 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
n14http://vocab.nerc.ac.uk/collection/P07/current/CFV8N128/4/
n7http://vocab.nerc.ac.uk/collection/P64/current/G963/
dctermshttp://purl.org/dc/terms/
dchttp://purl.org/dc/elements/1.1/
skoshttp://www.w3.org/2004/02/skos/core#
voidhttp://rdfs.org/ns/void#
n11http://vocab.nerc.ac.uk/collection/P02/current/TEMP/
n9http://vocab.nerc.ac.uk/standard_name/tendency_of_sea_water_temperature_due_to_horizontal_mixing/
n19http://vocab.nerc.ac.uk/collection/P06/current/KPRS/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
n5http://vocab.nerc.ac.uk/.well-known/
n18http://vocab.nerc.ac.uk/collection/P07/current/CFV8N128/1/
xsdhhttp://www.w3.org/2001/XMLSchema#
n13http://vocab.nerc.ac.uk/collection/P04/current/G963/
n16http://vocab.nerc.ac.uk/collection/P07/current/CFV8N128/2/
n3http://purl.org/pav/
n17http://vocab.nerc.ac.uk/collection/P07/current/CFV8N128/3/
n15http://mmisw.org/ont/cf/parameter/
n2http://vocab.nerc.ac.uk/collection/P07/current/CFV8N128/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
4
owl:sameAs
n9: n15:tendency_of_sea_water_temperature_due_to_horizontal_mixing
skos:broader
n7: n11: n13:
skos:prefLabel
tendency_of_sea_water_temperature_due_to_horizontal_mixing
dcterms:identifier
SDN:P07::CFV8N128
dc:identifier
SDN:P07::CFV8N128
dcterms:date
2024-05-20 20:39:49.0
skos:definition
The phrase "tendency_of_X" means derivative of X with respect to time. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Horizontal mixing" means any horizontal transport other than by advection and parameterized eddy advection, usually represented as horizontal diffusion in ocean models. 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. It is strongly recommended that a variable with this standard name should have the attribute units_metadata="temperature: difference", meaning that it refers to temperature differences and implying that the origin of the temperature scale is irrelevant, because it is essential to know whether a temperature is on-scale or a difference in order to convert the units correctly (cf. https://cfconventions.org/cf-conventions/cf-conventions.html#temperature-units).
skos:notation
SDN:P07::CFV8N128
skos:altLabel
owl:deprecated
false
skos:note
accepted
void:inDataset
n5:void
skos:related
n19:
n3:authoredOn
2024-05-20 20:39:49.0
n3:hasCurrentVersion
n14:
n3:hasVersion
n16: n17: n18:
n3:version
4