Methodological notes


Institute ofExperimental Meteorology, SPA Typhoon, ul. Pobedy 4, Obninsk, Kaluga Region, 249038, Russian Federation

A convective instability in a system of two immiscible fluids under gravity may arise not only from heating from below but also as a result of a horizontally uniform heating from above, i.e., with either fluid exhibiting a stable stratification. Some recently discovered mechanisms of such instability are discussed.

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Fulltext is also available at DOI: 10.1070/PU1997v040n07ABEH000256
PACS: 44.25.+f, 47.20.Bp (all)
DOI: 10.1070/PU1997v040n07ABEH000256
Citation: Ingel’ L Kh "'Anticonvection'" Phys. Usp. 40 741–745 (1997)
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:    «„“» 167 779–784 (1997); DOI: 10.3367/UFNr.0167.199707g.0779

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