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

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Namespace Prefixes

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n4http://vocab.nerc.ac.uk/collection/P07/current/CFV10N7/
n9http://vocab.nerc.ac.uk/standard_name/sea_water_x_velocity_due_to_parameterized_mesoscale_eddies/
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Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
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owl:sameAs
n4: n8:sea_water_x_velocity_due_to_parameterized_mesoscale_eddies n9:
skos:prefLabel
sea_water_x_velocity_due_to_parameterized_mesoscale_eddies
dcterms:identifier
SDN:P07::EISQFY55
dc:identifier
SDN:P07::EISQFY55
dcterms:date
2017-11-28 06:51:05.0
skos:definition
A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. 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_x_velocity_due_to_parameterized_mesoscale_eddies is used in some parameterisations of lateral diffusion in the ocean.
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