Concept
ocean_tracer_diffusivity_due_to_parameterized_mesoscale_eddy_advection
| URI | http://vocab.nerc.ac.uk/collection/P07/current/375L8O5D/1/ | ||
|---|---|---|---|
| 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 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 eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized mesoscale eddy advection occurs 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 eddy advection is represented in ocean models using schemes such as the Gent-McWilliams scheme. There are also standard names for parameterized_submesoscale_eddy_advection which, along with parameterized_mesoscale_eddy_advection, contributes to the total parameterized eddy advection. | ||
| Date | 2017-11-28T06:51:05 | ||
| Identifier | SDN:P07::375L8O5D | ||
| Note | accepted | ||
| Is Version Of | 375L8O5D | ||
| version | 1 | ||
| Same As | MMI | http://mmisw.org/ont/cf/parameter/ocean_tracer_diffusivity_due_to_parameterized_mesoscale_eddy_advection | |
| CF | http://vocab.nerc.ac.uk/standard_name/ocean_tracer_diffusivity_due_to_parameterized_mesoscale_eddy_advection/ | ||
| Related | P06:SQMS |
Square metres per second | |
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