The effect of intense radio waves on the formation of the midlatitude sporadic E-layer

Physics

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Ionospheric Heating, Midlatitude Atmosphere, Plasma Heating, Radio Frequency Heating, Sporadic E Layer, Electron Gas, Photochemical Reactions, Recombination Reactions, Wind Shear

Scientific paper

The effect of ionospheric plasma heating by an intense radio wave field on the formation of the midlatitude sporadic E-layer is studied on the basis of a wind shear model for the homogeneous heating of an electron gas. The formation of the sporadic E is associated with the redistribution of E-region ionization under the action of horizontal winds with sharp vertical velocity gradients. The model examines the effect of radio frequency heating on the maximal electron concentration and the width of the sporadic E-layer, taking account of changes in the ionization-recombination equilibrium, ion-photochemical processes, and the conditions of hydrodynamic equilibrium.

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