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. © 1971 D. Reidel Publishing Company.
CITATION STYLE
Obukhov, A. M. (1971). Turbulence in an atmosphere with a non-uniform temperature. Boundary-Layer Meteorology, 2(1), 7–29. https://doi.org/10.1007/BF00718085
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