Identification of the mechanisms responsible for anomalies in the tropical lower thermosphere/ionosphere caused by the January 2009 sudden stratospheric warming | Journal of Space Weather and Space Climate

Open Access

Fig. 5

EAGLE-simulated diurnal variations of the disturbances in zonal and meridional thermospheric wind (top panels) and Pedersen and Hall conductivities (bottom panels) on 27 January 2009 at the latitude range from 40° S to 40° N in the American longitudinal sector (75° W) and 120 km altitude.

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