ConceptDEPRECATED
ocean_tracer_bolus_biharmonic_diffusivity
URI | http://vocab.nerc.ac.uk/collection/P07/current/CF12N561/2/ | ||
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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. "Bolus diffusivity" means a lateral diffusivity. "biharmonic diffusivity" means diffusivity for use with a biharmonic diffusion operator. | ||
Date | 2017-11-28T06:51:07 | ||
Identifier | SDN:P07::CF12N561 | ||
Note | deprecated | ||
Is Version Of | CF12N561 | ||
Previous Version | 1 | ||
version | 2 | ||
Same As | P07:KHM9VKP7 |
ocean_tracer_biharmonic_diffusivity_due_to_parameterized_mesoscale_eddy_advection | |
MMI | http://mmisw.org/ont/cf/parameter/ocean_tracer_bolus_biharmonic_diffusivity | ||
CF | http://vocab.nerc.ac.uk/standard_name/ocean_tracer_bolus_biharmonic_diffusivity/ | ||
Related | P04:G915 |
EARTH SCIENCE > Oceans > Ocean Circulation > Diffusion | |
P64:G915 |
EARTH SCIENCE > Oceans > Ocean Circulation > Diffusion | ||
P06:M4S1 |
Metres to the power four per second |
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