Generalization of a Prandtl Slope Flow Model with a Heavy Admixture
- Authors: Ingel L.K.1,2
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Affiliations:
- “Taifun” Research and Production Association
- Obukhov Institute of Atmospheric Physics
- Issue: Vol 59, No 5 (2018)
- Pages: 857-861
- Section: Article
- URL: https://journals.rcsi.science/0021-8944/article/view/161319
- DOI: https://doi.org/10.1134/S0021894418050127
- ID: 161319
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Abstract
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.
Keywords
About the authors
L. Kh. Ingel
“Taifun” Research and Production Association; Obukhov Institute of Atmospheric Physics
Author for correspondence.
Email: lev.ingel@gmail.com
Russian Federation, Obninsk, 249038; Moscow, 119017
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