Concept
Sea water x velocity due to parameterized mesoscale eddies
URI | http://vocab.nerc.ac.uk/standard_name/sea_water_x_velocity_due_to_parameterized_mesoscale_eddies/ | ||
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Within Vocab | Climate and Forecast Standard Names | ||
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. | ||
Date | None | ||
Note | accepted | ||
modified | 2017-11-28 06:51:05.0 | ||
Exact Match | http://mmisw.org/ont/cf/parameter/sea_water_x_velocity_due_to_parameterized_mesoscale_eddies | ||
http://vocab.nerc.ac.uk/standard_name/sea_water_x_velocity_due_to_parameterized_mesoscale_eddies/ | |||
P07 Climate and Forecast Standard Names - (2) | |||
Related | P06:UVAA |
Metres per second |
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