Seasonal difference in ionization and height of F2-layer caused by neutrals at low latitudes

Physics

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Atmospheric Ionization, F 2 Region, Neutral Gases, Solar Activity Effects, Solar Terrestrial Interactions, Tropical Regions, Annual Variations, Diurnal Variations, Equatorial Electrojet, Summer, Winter

Scientific paper

Simulation of seasonal anomaly based on a morphological study at low latitudes is presented. Summer-winter differences are studied in the diurnal behavior of foF2 and hpF2 and in the strength of the equatorial electrojet for three low-latitude stations and three solar activity periods. Simultaneous examination of the equatorial electrojet strength of foF2 and hpF2 shows that the seasonal differences cannot be ascribed to the corresponding differences in the magnitude of the electromagnetic drift. Solving the continuity equation at low latitudes for a high solar activity period and assuming increased atomic oxygen in the summer, it is concluded that the seasonal differences in the foF2 are of the order of the observed seasonal differences.

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