atmosphere_obukhov_length
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.
List containing this term version:
CF (84)
CF (85)
CF (86)
Proposls with this term version:
Proposal: Nathan Anderson [Standard names: 7 New Flux Variables]
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