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Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

From: Relationship between day-to-day variability of equatorial plasma bubble activity from GPS scintillation and atmospheric properties from Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA) assimilation

Fig. 4

Longitudinal fluctuations in GAIA temperature averaged over 10 EPB-active days in each period. The periods and timing are a March and April 2003 and 1230 UT and b March and April 2004 and 1230 UT. Temperature perturbation is obtained as a deviation from the zonal 5-point running mean. Solid, dashed, and dotted lines in each panel are data at 4 N, 23 S, and 32 N latitudes, respectively

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