Evolution of atmospheric gravity waves in horizontal shear flow

The evolution of atmospheric gravity waves (AGW) in unbounded horizontal winds with constant shear is developed for the three-dimensional case. The atmosphere is considered to be isothermally stratified and the wind shear lies in the horizontal plane. Time varying frequencies of the AGW, which for large times tends to the isothermal Brunt-Vaisala frequency is obtained. The excitation of vortical perturbations located in the horizontal plane shear waves, is shown. The time variation of AGW frequencies, the existence of shear wave and their amplitudes amplification/damping are due to the presence of the horizontal shear flow. The horizontal shear flow as a possible source of formation of large scale travelling ionospheric disturbances (TIDs) with small period (16 - 19 min) is considered. The different pictures of evolution of the AGW like initial perturbation are obtained in vertical, horizontal winds and its shear directions. The importance of coupling between the gravity and shear waves in the horizontal shear how is shown. The possibility of transformation of shear waves into AGWs is demonstrated.