This HTML5 document contains 19 embedded RDF statements represented using HTML+Microdata notation.

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Namespace Prefixes

PrefixIRI
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n3http://purl.org/pav/
n12http://vocab.nerc.ac.uk/standard_name/sea_water_y_velocity_due_to_parameterized_mesoscale_eddies/
n14http://mmisw.org/ont/cf/parameter/
n2http://vocab.nerc.ac.uk/collection/P07/current/J0OEZBJ5/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
1
owl:sameAs
n9: n12: n14:sea_water_y_velocity_due_to_parameterized_mesoscale_eddies
skos:prefLabel
sea_water_y_velocity_due_to_parameterized_mesoscale_eddies
dcterms:identifier
SDN:P07::J0OEZBJ5
dc:identifier
SDN:P07::J0OEZBJ5
dcterms:date
2017-11-28 06:51:05.0
skos:definition
A velocity is a vector quantity. "y" indicates a vector component along the grid y-axis, positive with increasing y. 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. Parameterized mesoscale eddies occur on a spatial scale of many tens of kilometres and an evolutionary time of weeks. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. Parameterized mesoscale eddies are represented in ocean models using schemes such as the Gent-McWilliams scheme. sea_water_y_velocity_due_to_parameterized_mesoscale_eddies is used in some parameterisations of lateral diffusion in the ocean.
skos:notation
SDN:P07::J0OEZBJ5
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false
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n10:
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