This HTML5 document contains 25 embedded RDF statements represented using HTML+Microdata notation.

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Namespace Prefixes

Prefix	IRI
n2	http://vocab.nerc.ac.uk/collection/P07/current/CFSN0827/
dcterms	http://purl.org/dc/terms/
n18	http://vocab.nerc.ac.uk/collection/P04/current/G920/
n15	http://vocab.nerc.ac.uk/collection/P02/current/RFVL/
n14	http://vocab.nerc.ac.uk/collection/P64/current/G920/
dc	http://purl.org/dc/elements/1.1/
n13	http://vocab.nerc.ac.uk/collection/P06/current/UVAA/
skos	http://www.w3.org/2004/02/skos/core#
void	http://rdfs.org/ns/void#
n7	http://vocab.nerc.ac.uk/standard_name/surface_geostrophic_sea_water_x_velocity_assuming_sea_level_for_geoid/
rdf	http://www.w3.org/1999/02/22-rdf-syntax-ns#
n10	http://vocab.nerc.ac.uk/.well-known/
owl	http://www.w3.org/2002/07/owl#
n19	http://vocab.nerc.ac.uk/collection/P07/current/CFSN0827/1/
n16	http://vocab.nerc.ac.uk/collection/P07/current/CFSN0827/2/
n20	http://vocab.nerc.ac.uk/collection/P07/current/R33VVM5P/
xsdh	http://www.w3.org/2001/XMLSchema#
n17	http://vocab.nerc.ac.uk/collection/P07/current/CFSN0827/3/
n4	http://purl.org/pav/
n8	http://mmisw.org/ont/cf/parameter/
n12	http://vocab.nerc.ac.uk/collection/P07/current/CFSN0827/4/

Statements

Subject Item

n2:

rdf:type

skos:Concept

owl:versionInfo

4

owl:sameAs

n7: n8:surface_geostrophic_sea_water_x_velocity_assuming_sea_level_for_geoid n20:

skos:broader

n14: n15: n18:

skos:prefLabel

surface_geostrophic_sea_water_x_velocity_assuming_sea_level_for_geoid

dcterms:identifier

SDN:P07::CFSN0827

dc:identifier

SDN:P07::CFSN0827

dcterms:date

2017-06-26 15:24:30.0

skos:definition

The surface called "surface" means the lower boundary of the atmosphere. A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. "Geostrophic" indicates that geostrophic balance is assumed, i.e. that the pressure gradient force and the Coriolis force are balanced and the large scale fluid flow is parallel to the isobars. "sea_level" means mean sea level. The geoid is a surface of constant geopotential with which mean sea level would coincide if the ocean were at rest. (The volume enclosed between the geoid and the sea floor equals the mean volume of water in the ocean.) In an ocean GCM the geoid is the surface of zero depth, or the rigid lid if the model uses that approximation. surface_geostrophic_sea_water_x_velocity_assuming_sea_level_for_geoid is the variable part of surface_geostrophic_sea_water_x_velocity. The assumption that sea level is equal to the geoid means that the stationary component of ocean circulation is equal to zero.

skos:notation

SDN:P07::CFSN0827

skos:altLabel

owl:deprecated

true

skos:note

deprecated

void:inDataset

n10:void

skos:related

n13:

n4:authoredOn

2017-06-26 15:24:30.0

n4:hasCurrentVersion

n12:

n4:hasVersion

n16: n17: n19:

n4:version

4