Concept
ocean_obukhov_length
URI | http://vocab.nerc.ac.uk/collection/P07/current/GQ9G6TH3/1/ | ||
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Within Vocab | Climate and Forecast Standard Names | ||
Alternative Labels | |||
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 | 2024-01-18T09:01:44 | ||
Identifier | SDN:P07::GQ9G6TH3 | ||
Note | accepted | ||
Is Version Of | GQ9G6TH3 | ||
version | 1 | ||
Same As | MMI | http://mmisw.org/ont/cf/parameter/ocean_obukhov_length | |
CF | http://vocab.nerc.ac.uk/standard_name/ocean_obukhov_length/ | ||
Related | P06:ULAA |
Metres |
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