The behaviour of the topside ionosphere during storm conditions

Physics

Scientific paper

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Scientific paper

The behaviour of the topside ionosphere during five different storms is discussed; certain features of the observed behaviour appear so consistently that it seems possible to make several generalizations about the storm behaviour of the topside ionosphere. The storm effects are much more pronounced at the lower heights where the electron concentration varies by up to a factor of four. The evidence suggests that the effects are due more to a vertical movement of the layer than to a primary change in NmF2. The storm effects vary markedly with latitude, being more [`]positive' at lower latitudes; [`]negative' storms occur at higher latitudes. Evidence is also given which indicates that sometimes the storm effects are positive shortly after the magnetic SC, but become negative later.

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