Spread-F and the parameters of the F-layer of the ionosphere--IV0

Physics

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Scientific paper

The impact of the results of the previous parts of this series on the several theories of spread-F irregularity production is discussed. It is found impossible to reconcile the results with four of these theories, namely, 's instability of the under surface of an upward drifting layer, 's E-region turbulence communicated to the F-layer, and 's convective motion of the magnetosphere and a theory of auroral particle origin of the irregularities. A new theory, based on initiation of instability of the surfaces of a drifting layer by hydromagnetic waves, is proposed. It is shown that this theory is in accord with the experimental findings.

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