Concept
ocean_vertical_momentum_diffusivity_due_to_background
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CF12N567/2/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| 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. | ||
| Date | 2019-02-04T14:52:1 | ||
| Identifier | SDN:P07::CF12N567 | ||
| Note | accepted | ||
| Is Version Of | CF12N567 | ||
| Previous Version | 1 | ||
| version | 2 | ||
| Same As | MMI | http://mmisw.org/ont/cf/parameter/ocean_vertical_momentum_diffusivity_due_to_background | |
| CF | http://vocab.nerc.ac.uk/standard_name/ocean_vertical_momentum_diffusivity_due_to_background/ | ||
| Related | P04:G915 |
EARTH SCIENCE > Oceans > Ocean Circulation > Diffusion | |
P64:G915 |
EARTH SCIENCE > Oceans > Ocean Circulation > Diffusion | ||
P06:SQMS |
Square metres per second | ||
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