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Fig. 4

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EAGLE-simulated diurnal variations of the meridional (top panel) and zonal (middle panel) electric field disturbances on 27 January 2009 at 40° S–40° N latitudes in the American longitudinal sector (75° W) and 175 km altitude. The bottom panel presents the zonal electric field disturbances that were obtained with the stand-alone GSM TIP model using the TIME-GCM model output with an additional electric potential that allowed for the reproduction of TEC disturbances during the 2009 SSW event (Klimenko et al., 2015).

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