Publisher's Synopsis
Excerpt from Asymptotic Behavior of Planetary-Scale Motions of the Atmosphere
In this paper we derive approximate equations describing adiabatic planetary - scale motions of the atmosphere valid for asymptotically large time from the viewpoint of the original fluid equations. Although this approximation procedure yields an ordered system of linear partial differential equations, the coefficients are variable; and numerical calculations must be carried out in the future in order to verify if the actual physical atmosphere allows such motions to exist.
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