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Responses of ionospheric F 2 peak to three types of meridional winds, namely constant winds, Servo Model-based winds and HWM-90 winds, are investigated numerically for Wuchang (30. 5 o N, 114. 4 o E) and Wakkanai (45. 5 o N, 141. 7 o E), with the help of a theoretical model for one-dimensional and time-dependent ionospheric profile.
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