Abstract

Studies of the intensity of horizontal drift velocity perturbations with periods 0.7 – 3 hours at the altitudes 80 – 110 km are made from the data of regular low-frequency D1 ionospheric reflection observations at Collm, Germany (52° N, 15° E) in 1983 – 1999. Seasonal changes of variances of short-period perturbations of zonal velocity reveal the main maximum in summer and a smaller maximum in winter near the altitude 80 km and the two maxim at equinoxes near and above 100 km. Perturbation variances had the minima in 1985 -- 1987 and in 1996 -- 1998. Numerical modeling shows that IGW's generated in the strato-mesospheric jet stream may have substantial amplitudes at altitudes near and above 100 km and may modify seasonal variations of tropospheric IGWs.

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