Monin–Obukhov similarity theory

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Monin–Obukhov similarity theory is a foundational framework in boundary-layer meteorology that describes how turbulence and mean profiles of wind, temperature, and other scalars scale in the atmospheric surface layer under varying stability conditions.

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Monin–Obukhov similarity theory canonical 1

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von Kármán constant usedIn Monin–Obukhov similarity theory