Concept
upward_sea_water_velocity_due_to_parameterized_mesoscale_eddies
| URI | http://vocab.nerc.ac.uk/collection/P07/current/J1F4A574/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | A velocity is a vector quantity. "Upward" indicates a vector component which is positive when directed upward (negative downward). 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. | ||
| Date | 2017-11-28T06:51:05 | ||
| Identifier | SDN:P07::J1F4A574 | ||
| Note | accepted | ||
| Has Current Version | 1 | ||
| version | 1 | ||
| Same As | P07:CFV8N6 |
bolus_upward_sea_water_velocity | Mapping: 1410285 |
| MMI | http://mmisw.org/ont/cf/parameter/upward_sea_water_velocity_due_to_parameterized_mesoscale_eddies | Mapping: 310479 | |
| CF | http://vocab.nerc.ac.uk/standard_name/upward_sea_water_velocity_due_to_parameterized_mesoscale_eddies/ | Mapping: 367277 | |
| Related | P06:UVAA |
Metres per second | Mapping: 1410286 |
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