Concept
ocean_kinetic_energy_dissipation_per_unit_area_due_to_vertical_friction
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CF12N546/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | Friction, leading to the dissipation of kinetic energy, arises in ocean models as a result of the viscosity of sea water. Generally, the lateral (xy) viscosity is given a large value to maintain the numerical stability of the model. In contrast, the vertical viscosity is usually much smaller. 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. | ||
| Date | 2009-07-06T15:41:29 | ||
| Identifier | SDN:P07::CF12N546 | ||
| Note | accepted | ||
| Has Current Version | 1 | ||
| version | 1 | ||
| Same As | MMI | http://mmisw.org/ont/cf/parameter/ocean_kinetic_energy_dissipation_per_unit_area_due_to_vertical_friction | Mapping: 253772 |
| CF | http://vocab.nerc.ac.uk/standard_name/ocean_kinetic_energy_dissipation_per_unit_area_due_to_vertical_friction/ | Mapping: 357589 | |
| Related | P02:VDFC |
Transport in the water column | Mapping: 167928 |
P06:UFAA |
Watts per square metre | Mapping: 164496 | |
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