Abstract
The temperature of the mesopause region (87 km) is monitored at the Maimaga station (63.04 ° N, 129.51 ° E) using the Shamrock (Andor) spectrograph recording the hydroxyl (OH) band (3, 1). The temperature data obtained for the seasons from 2013 to 2017 are investigated. The standard deviations corresponding to the internal gravity σgw and tidal waves σtd were obtained. The seasonal course of the tidal component σtd varies from 2 to 5 K throughout all observation seasons. The seasonal variation of the gravitational component σgw observed at Maimaga station almost coincides for three observation seasons except for the 2014-2015 season. In this observation season, σgw has lower values in winter than in other seasons. Moreover, in this season average monthly temperatures exceed similar values in other seasons.
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