Spectral energy contributions of quasi-periodic oscillations (2-35 days) to the variability of the f sub(o) F2

The relative contributions of quasi-periodic oscillations from 2 to 35 days to the variability of [f] sub(o) F2 at middle northern latitudes between 42 degrees N and 60 degrees N are investigated. The [f] sub(o) F2 hourly data for the whole solar cycle 21 (1976-1986) for four European ionospheric stations Rome (41.9 degrees N, 12.5 degrees E), Poitiers (46.5 degrees N, 0.3 degrees E), Kaliningrad (54.7 degrees N, 20.6 degrees E) and Uppsala (59.8 degrees N, 17.6 degrees E) are used for analysis. The relative contributions of different periodic bands due to planetary wave activity and solar flux variations are evaluated by integrated percent contributions of spectral energy for these bands. The observations suggest that a clearly expressed seasonal variation of percent contributions exists with maximum at summer solstice and minimum at winter solstice for all periodic bands. The contributions for summer increase when the latitude increases. The contributions are modulated by the solar cycle and simultaneously influenced by the long-term geomagnetic activity variations. The greater percentage of spectral energy between 2 to 35 days is contributed by the periodic bands related to the middle atmosphere planetary wave activity.