A variable K planetary boundary-layer model

Details A variable K planetary boundary-layer model A variable K planetary boundary-layer model

Jan 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977bolme..11..117m&link_type=abstract

Boundary-Layer Meteorology, Volume 11, Issue 1, pp.117-120

Computer Science

1

Scientific paper

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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