About: tendency_of_sea_water_temperature_due_to_bolus

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Attributes	Values
type	Concept
versionInfo	3
sameAs	tendency_of_sea_water_temperature_due_to_bolus_advection tendency_of_sea_water_temperature_due_to_bolus_advection tendency_of_sea_water_temperature_due_to_bolus_advection
has broader	http://vocab.nerc.ac.uk/collection/P02/current/TEMP/ sea_water_temperature sea_water_temperature
preferred label	tendency_of_sea_water_temperature_due_to_bolus_advection (en)
Identifier	SDN:P07::CFV8N127
dc:identifier	SDN:P07::CFV8N127
Date	2017-11-28 06:51:07.0
definition	"tendency_of_X" means derivative of X with respect to time. Bolus advection in an ocean model means the part due to a scheme representing eddy-induced effects not included in the velocity field. 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. 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. (en)
notation	SDN:P07::CFV8N127
alternative label
owl:deprecated	true
note	deprecated (en)
void:inDataset	http://vocab.nerc.ac.uk/.well-known/void
has related	http://vocab.nerc.ac.uk/collection/P06/current/KPRS/
http://purl.org/pav/authoredOn	2017-11-28 06:51:07.0
http://purl.org/pav/hasCurrentVersion	http://vocab.nerc.ac.uk/collection/P07/current/CFV8N127/3/
http://purl.org/pav/hasVersion	http://vocab.nerc.ac.uk/collection/P07/current/CFV8N127/1/ http://vocab.nerc.ac.uk/collection/P07/current/CFV8N127/2/
http://purl.org/pav/version	3
is sameAs of	tendency_of_sea_water_temperature_due_to_bolus_advection tendency_of_sea_water_temperature_due_to_bolus_advection
is has member of	Climate and Forecast Standard Names

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