Medium scale structure of the F-region.

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Earth Ionosphere: F Region, Earth Ionosphere: Variations

Scientific paper

Digital ionograms recorded during 1980/81 at Brighton, Colorado show characteristics (e.g. virtual height variations and doppler profiles) supporting the hypothesis that short term F-region variations are caused by acoustic gravity waves which seem to be present all the time with varying amplitudes. In addition, some direct evidence for the spatial structure can be obtained from the angle of arrival observations and their frequency or height dependence. Comparisons of foF2 and MUF (3000) indicate that the main effect of gravity waves on the F-region structure is the variation of the height of the layer and to a lesser degree a variation of the maximum electron density.

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