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Figure 4 Variation of electron density profile.

Figure 6 presents the seasonal variation of electron density profiles obtained by different methods.

Variation of electron fluxes and Kp and Dst indices within selected intervals for other anomaly cases given in Table 4.

The variation of electron density in the ionosphere has significant effects on a radio signal propagating through the Earth's atmosphere.

The seasonal variation of electron density profile in the study of Maurya et al. (2012a) shows more significance.

This behavior may be attributed to latitudinal variation of electron density, well known as the Equatorial Ionization Anomaly (EIA).

This conclusion was also confirmed by our calculations using van Oss-Chaudhury-Good approach [34], which showed dramatic variation of electron-acceptor component related to a polar sort of surface interactions.

Monthly mean variations of electron density profiles are discussed for Wakkanai and Poker Flat.

Thus, the periodic field-aligned electron flux produces local variations of electron density in the E-layer and bottom of the F-layer.

The main focuses of the paper is to see the diurnal, seasonal and latitudinal variations of electron and ion temperatures during periods of minimum to maximum solar activity.

Through impedance spectroscopy, we have evaluated quantitatively the effects of shifts in the conduction band energy level and variations of electron recombination rates over the photovoltage.