Concept
Ocean obukhov length
| URI | http://vocab.nerc.ac.uk/standard_name/ocean_obukhov_length/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Definition | The depth in the ocean, L, that buoyant production or destruction of turbulent energy balances the turbulent kinetic energy: L = -u*3 / (kB0), where u* is the oceanic surface frictional velocity, k is the von Karman constant, and B0 is the oceanic surface buoyancy flux. If the buoyancy flux is destabilizing, L is negative. | ||
| Date | None | ||
| Note | accepted | ||
| modified | 2024-01-18 09:01:44.0 | ||
| Exact Match | http://mmisw.org/ont/cf/parameter/ocean_obukhov_length | ||
| http://vocab.nerc.ac.uk/standard_name/ocean_obukhov_length/ | |||
P07:GQ9G6TH3 |
ocean_obukhov_length | ||
| Related | P06:ULAA |
Metres | |
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