Abstract
The stability of the Ekman thermally stratified boundary layer simulating the atmospheric boundary layer is studied theoretically. The system of thermohydrodynamic equations is solved in the Boussinesq approximation. Two mechanisms of development of the vortex structures, namely, thermal and dynamic, as well as their interaction, are investigated. It is shown that a sharp boundary on which the flow characteristics change qualitatively exists between various domains of the parameters corresponding to thermal and dynamic instabilities.
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Additional information
Moscow. Translated from Izvestiya Rossiiskoi Akademii Nauk, Mekhanika Zhidkosti i Gaza, No. 3, pp. 71–76, May–June, 1998.
The work was carried out with financial support from the Russian Foundation for Basic Research (project No. 96-01-01118).
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Ordanovich, A.E., Pashkovskaya, Y.V. Effect of thermal stratification on ekman flow stability. Fluid Dyn 33, 355–359 (1998). https://doi.org/10.1007/BF02698185
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DOI: https://doi.org/10.1007/BF02698185