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A variable K planetary boundary-layer model
Authors:Prasanta K Misra
Institution:(1) Whiteshell Nuclear Research Establishment, Atomic Energy of Canada Limited, Pinawa, Man., Canada
Abstract:The steady-state, homogeneous and barotropic equations of motion within the planetary boundary layer are solved with the assumption that the coefficient of eddy viscosity varies as K(Z) = K O(1–Z/h) p , where h is the height of the bounday layer and p is a parameter which depends on atmospheric stability. The solutions compare favourably with observed velocity profiles based on the Wangara data.
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