ocean_obukhov_length

https://w3id.org/hacid/data/cs/variables/cf/ocean_obukhov_length <https://w3id.org/hacid/onto/data/Variable>

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. rdf:langString

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rdf:langString ocean_obukhov_length

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