# Monin-obukhov similarity theory

From Glossary of Meteorology

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## Monin–Obukhov similarity theory

A relationship describing the vertical behavior of nondimensionalized mean flow and turbulence properties within the atmospheric surface layer (the lowest 10% or so of the atmospheric boundary layer) as a function of the Monin–Obukhov key parameters.

These key parameters are the height where 2) a surface-layer temperature scale, 3) a length scale called the Obukhov length, where where

*z*above the surface, the buoyancy parameter ratio*g*/*T*_{v}of inertia and buoyancy forces, the kinematic surface stress τ_{0}/ρ, and the surface virtual temperature flux*g*is gravitational acceleration,*T*_{v}is virtual temperature, τ_{0}is turbulent stress at the surface, ρ is air density,*Q*_{v0}is a kinematic virtual heat flux at the surface,*H*_{v0}is a dynamic virtual heat flux at the surface,*C*_{p}is the specific heat of air at constant pressure, and is the covariance of vertical velocity*w*with virtual temperature near the surface. The key parameters can be used to define a set of four dimensional scales for the surface layer: 1) the friction velocity or shearing velocity, a velocity scale,*k*is the von Kármán constant; and 4) the height above ground scale,*z*. These key scales can then be used in dimensional analysis to express all surface-layer flow properties as dimensionless universal functions of*z*/*L*. For example, the mean wind shear in any quasi-stationary, locally homogeneous surface layer can be written as*f*is a universal function of the dimensionless height*z*/*L*. The forms of the universal functions are not given by the Monin–Obukhov theory, but must be determined theoretically or empirically. Monin–Obukhov similarity theory is the basic similarity hypothesis for the horizontally homogeneous surface layer. With these equations and the hypothesis that the fluxes in the surface layer are uniform with height, the momentum flux, sensible heat flux, and fluxes of water vapor and other gases can be determined.*Compare*aerodynamic roughness length, Richardson number.