Magnetic declination control of the equatorial F region dynamo electric field development and spread F

Physics

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Dynamo Theory, Equatorial Regions, F Region, Ionospheric Drift, Magnetic Variations, Spread F, Atmospheric Ionization, Diurnal Variations, Drift Rate, Electric Fields, Radar Measurement

Scientific paper

A comparative study of evening prereversal enhancements in equatorial F region vertical ionization drift velocities conducted over two magnetic equatorial stations, at 4 deg S, 38 deg N and 12 deg S, 77 deg W, shows dissimilarities in the seasonal trends of the drift velocity prereversal peak times and widths. The dissimilarities, which are also reflected in spread F characteristics, are shown to be mainly due to the difference in magnetic field declination angle. This difference causes (1) differences in the conjugate E region sunset durations, and, in turn, in (2) the F region polarization electric field development rates at the two stations.

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