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The dispersing equation was derived from system of the hydrodynamic equationsthat take into account the gravity, and from boundary conditions of shockfront. The dispersing equation made it possible to study unstable stability offront not only relative to sound vibrations, but also to explore thegravitational branch of acousto-gravitational waves. Within the framework ofthe model under study there appeared a possibility to examine the interval offrequencies in which wave disturbances of the aerosphere induced by shock wavesfrom land-based sources are energized.

On The Procedure Of Examination Of Instability Of The Shock Front Relatively Acousto-Gravitational Perturbations