On one mechanism of gravity field inhomogeneities influence on atmosphere dynamics


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Abstract

Taking into account the heat exchange, the horizontal inhomogeneities of the gravity field were shown to lead to the origin of dynamic perturbations (flows) in the density stratified medium. The amplitude of the horizontal component of the originating flows is proportional to the product of a geoid deviation from a uniform Earth ellipsoid and buoyancy frequency.

About the authors

L. Kh. Ingel’

Typhoon Research and Production Association; Obukhov Institute of Atmospheric Physics

Author for correspondence.
Email: lev.ingel@gmail.com
Russian Federation, Obninsk, Kaluga oblast, 249038; Moscow, 119017

A. A. Makosko

Obukhov Institute of Atmospheric Physics

Email: lev.ingel@gmail.com
Russian Federation, Moscow, 119017

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