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These observed features and many others were hitherto explained on the basis of equatorial plasma dynamics associated with the Appleton ionization anomaly (EIA Equatorial Ionization Anomaly).
During solar cycle 24 in 2013, equatorial ionization anomaly (EIA) leads to affecting annual and semiannual.
Occurrence of scintillation does happen at and around the ionization anomaly crest over Kenyan region.
These locations coincide with the southern part of the Equatorial Ionization Anomaly crest over Kenya region.
Latitudinal variation of TEC shows development of strong Equatorial Ionization Anomaly (EIA) on the recovery phase.
This behavior may be attributed to latitudinal variation of electron density, well known as the Equatorial Ionization Anomaly (EIA).
The main aspects of the reconstruction results at the equatorial ionization anomaly (EIA) region over Brazil are highlighted and discussed.
It is also observed that the most profound saturation effect appears at the equatorial ionization anomaly crest region.
Daytime eastward prompt penetration electric fields, if they occur, also shift the Equatorial Ionization Anomaly (EIA) crests to higher than normal latitudes.
Zhao et al. (2005) investigated the response of the Equatorial Ionization Anomaly (EIA) to the superstorms of October November 2003 using GPS data measured over a regional area.
The TEC variability of the post sunset hours is associated with the occurrence of the ionization anomaly crest which enhances nighttime TEC over this region.
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