Concept
atmosphere_obukhov_length
| URI | http://vocab.nerc.ac.uk/collection/P07/current/3DN55MN7/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | The height in the atmosphere, L, that buoyant production or destruction of turbulent energy balances the shear production of turbulent kinetic energy: L = -u*3 / (kB0), where u* is the wind frictional velocity, k is the von Karman constant, and B0 is the atmospheric surface buoyancy flux. If the buoyancy flux is destabilizing, L is negative. | ||
| Date | 2024-01-18T09:01:44 | ||
| Identifier | SDN:P07::3DN55MN7 | ||
| Note | accepted | ||
| Has Current Version | 1 | ||
| version | 1 | ||
| Same As | MMI | http://mmisw.org/ont/cf/parameter/atmosphere_obukhov_length | Mapping: 436297 |
| CF | http://vocab.nerc.ac.uk/standard_name/atmosphere_obukhov_length/ | Mapping: 436640 | |
| Related | P06:ULAA |
Metres | Mapping: 1791580 |
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