Generalization of a Prandtl Slope Flow Model with a Heavy Admixture


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Resumo

A Prandtl slope flow model is generalized for the case with a homogeneous stationary source of a heavy admixture that significantly changes the medium density. A stationary analytical solution for a velocity of arising flows, temperature deviations, and admixture distribution is obtained. The model describes, for example, some special features of the dynamics of a ground snowstorm above a slope surface.

Sobre autores

L. Ingel

“Taifun” Research and Production Association; Obukhov Institute of Atmospheric Physics

Autor responsável pela correspondência
Email: lev.ingel@gmail.com
Rússia, Obninsk, 249038; Moscow, 119017

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