Annotation
We consider an approximate mathematical model which takes into account the main factors in the interaction of the ocean and the atmosphere It is found that, in the framework of the present model, a temperature inversion layer Is formed by the action of volume heat sources in the atmosphere.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
A.A. Budnikov
Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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