Abstract
The mechanism of generation of a nonstationary large-scale high-intensity cyclonic vortex, which does not require for its origination the rotation of the cavity or the presence of a local heat source at the bottom, is described on the basis of experimental results.
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Original Russian Text © A.N. Sharifulin, A.N. Poludnitsin, A.S. Kravchuk, 2008, published in Zhurnal Éksperimental’noĭ i Teoreticheskoĭ Fiziki, 2008, Vol. 134, No. 6, pp. 1269–1273.
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Sharifulin, A.N., Poludnitsin, A.N. & Kravchuk, A.S. Laboratory-scale simulation of nonlocal generation of a tropical cyclone. J. Exp. Theor. Phys. 107, 1090–1093 (2008). https://doi.org/10.1134/S1063776108120170
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DOI: https://doi.org/10.1134/S1063776108120170