Rossby waves and cascade phenomena

M. Yu. Reshetnyak1
1Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia

Tóm tắt

Nonlinear triad interactions in the Navier-Stokes equation describing quasi-geostrophic thermal convection in a spherical layer are considered. The analysis provides an insight into the nature of kinetic energy transfer across the spectrum and allows us to assess the degree of nonlocality in the energy transfer. The distinguishing feature of the spherical problem is the emergence of the Rossby waves, which cause nonlocal redistribution of energy in the system. The results of this study are compared with their counterparts for the plane model.

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