Monin–Obukhov length
The Obukhov length is used to describe the effects of buoyancy on turbulent flows, particularly in the lower tenth of the atmospheric boundary layer. It was first defined by Alexander Obukhov in 1946. It is also known as the Monin–Obukhov length because of its important role in the similarity theory developed by Monin and Obukhov. A simple definition of the Monin-Obukhov length is that height at which turbulence is generated more by buoyancy than by wind shear. The Obukhov length is defined by where is the frictional velocity, is the mean virtual potential temperature, where is specific humidity.
primaryTopic
Monin–Obukhov length
The Obukhov length is used to describe the effects of buoyancy on turbulent flows, particularly in the lower tenth of the atmospheric boundary layer. It was first defined by Alexander Obukhov in 1946. It is also known as the Monin–Obukhov length because of its important role in the similarity theory developed by Monin and Obukhov. A simple definition of the Monin-Obukhov length is that height at which turbulence is generated more by buoyancy than by wind shear. The Obukhov length is defined by where is the frictional velocity, is the mean virtual potential temperature, where is specific humidity.
has abstract
La longueur d'Obukhov (L) est ...... veloppée par Monin et Obukhov.
@fr
O comprimento de Obukhov é uti ...... à produção cisalhante de ECT).
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The Obukhov length is used to ...... ind (shear production of TKE).
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Wikipage page ID
Wikipage revision ID
740,668,392
comment
La longueur d'Obukhov (L) est ...... veloppée par Monin et Obukhov.
@fr
O comprimento de Obukhov é uti ...... potencial, Por esta definição,
@pt
The Obukhov length is used to ...... e, where is specific humidity.
@en
label
Comprimento de Monin-Obukhov
@pt
Longueur de Monin-Obukhov
@fr
Monin–Obukhov length
@en