Turbulence in an atmosphere with a non-uniform temperature - Boundary-Layer Meteorology
- ️Obukhov, A. M.
- ️Mon Mar 01 1971
Abstract
In this work the effect of static stability on the development of atmospheric turbulence is investigated. This influence is considered quantitatively by generalizing Prandtl's semi-empirical theory, i.e., by using a correcting factor in the form of a universal function of the Richardson number. An evaluation of the thickness of the layer of dynamic turbulence under various external conditions is successfully achieved quantitatively.
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References
Brunt, D.: 1941,Physical and Dynamical Meteorology, Cambridge University Press, London.
Goldstein, S.: 1938,Modern Developments in Fluid Dynamics, Vol.2, Oxford University Press.
Keller, L. V.: 1930, ‘Theory of Convection and Turbulence’,Trudy Glavn. Geofis. Observ. (Works of Main Geophys. Observ.), No. 4.
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Authors and Affiliations
The Institute of Theoretical Geophysics of the Academy of Sciences of the U.S.S.R., Moscow, Russia
A. M. Obukhov
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- A. M. Obukhov
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In 1947 this Institute was transformed into Geophysical Institute. The latter in 1956 was divided into three parts, in one of which (Institute of Atmospheric Physics of the Academy of Sciences of the U.S.S.R.) A. M. Obukhov is serving as Director.
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Obukhov, A.M. Turbulence in an atmosphere with a non-uniform temperature. Boundary-Layer Meteorol 2, 7–29 (1971). https://doi.org/10.1007/BF00718085
Received: 01 April 1971
Issue Date: March 1971
DOI: https://doi.org/10.1007/BF00718085