About: ocean_vertical_tracer_diffusivity_due_to

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type	Concept
versionInfo	2
sameAs	ocean_vertical_tracer_diffusivity_due_to_background ocean_vertical_tracer_diffusivity_due_to_background
preferred label	ocean_vertical_tracer_diffusivity_due_to_background (en)
Identifier	SDN:P07::CF12N570
dc:identifier	SDN:P07::CF12N570
Date	2019-02-04 14:52:10.0
definition	Diffusivity is also sometimes known as the coefficient of diffusion. Diffusion occurs as a result of a gradient in the spatial distribution of mass concentration, temperature or momentum. The diffusivity may be very different in the vertical and horizontal directions. The construction "vertical_X_diffusivity" means the vertical component of the diffusivity of X due to motion which is not resolved on the grid scale of the model. 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. "Due to background" means caused by a time invariant imposed field which may be either constant over the globe or spatially varying, depending on the ocean model used. (en)
notation	SDN:P07::CF12N570
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owl:deprecated	false
note	accepted (en)
void:inDataset	http://vocab.nerc.ac.uk/.well-known/void
has related	http://vocab.nerc.ac.uk/collection/P04/current/G915/ http://vocab.nerc.ac.uk/collection/P06/current/SQMS/ http://vocab.nerc.ac.uk/collection/P64/current/G915/
http://purl.org/pav/authoredOn	2019-02-04 14:52:10.0
http://purl.org/pav/hasCurrentVersion	http://vocab.nerc.ac.uk/collection/P07/current/CF12N570/2/
http://purl.org/pav/hasVersion	http://vocab.nerc.ac.uk/collection/P07/current/CF12N570/1/
http://purl.org/pav/version	2
is has member of	Climate and Forecast Standard Names

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