Some results of S-transform analysis of the transient planetary-scale windoscillations in the lower thermosphere

Technique appropriate to the analysis of lower thermospheric wind data reco rded by global-scale networks of ground-based instruments are discussed. Th e S-transform technique is shown to be effective in the analysis of the mai n features of travelling planetary waves and this method is applied to the time series of horizontal-velocity data obtained during the DYANA campaign (January-March, 1990), The analysis reveals strongly transient behavior of the day-to-day lower thermosphere wind variations, as well as their specifi c longitudinal structure. In particular, it was found that the revealed qua si-15 day and quasi-5 day wind oscillations may be described as transient w estward-propagating waves with zonal wavenumber s = 1, while an oscillation with the a period near 7 days is tentatively identified as having a wavenu mber s = 0.