About: sea_water_velocity_to_direction_due_to_ekman

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About: sea_water_velocity_to_direction_due_to_ekman_drift Goto Sponge NotDistinct Permalink

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type	Concept
versionInfo	1
sameAs	sea_water_velocity_to_direction_due_to_ekman_drift sea_water_velocity_to_direction_due_to_ekman_drift
preferred label	sea_water_velocity_to_direction_due_to_ekman_drift (en)
Identifier	SDN:P07::L3CP5I62
dc:identifier	SDN:P07::L3CP5I62
Date	2024-05-20 20:39:48.0
definition	A velocity is a vector quantity. The phrase "to_direction" is used in the construction X_to_direction and indicates the direction towards which the velocity vector of X is headed. The direction is a bearing in the usual geographical sense, measured positive clockwise from due north. 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. "Ekman drift" is the movement of a layer of water (the Ekman layer) due to the combination of wind stress at the sea surface and the Coriolis effect. Ekman drift is to the right of the wind direction in the Northern Hemisphere and the left in the Southern Hemisphere. Reference: https://www.open.edu/openlearn/science-maths-technology/the-oceans/content-section-4.3. (en)
notation	SDN:P07::L3CP5I62
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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/P06/current/UAAA/
http://purl.org/pav/authoredOn	2024-05-20 20:39:48.0
http://purl.org/pav/hasCurrentVersion	http://vocab.nerc.ac.uk/collection/P07/current/L3CP5I62/1/
http://purl.org/pav/version	1
is sameAs of	sea_water_velocity_to_direction_due_to_ekman_drift
is has member of	Climate and Forecast Standard Names

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