Horizontal drifts accompanying large vertical motions of the nocturnal F-region

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Scientific paper

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Abstract

A large scale vertical convection of the mid dip-latitude post-midnight F-region of the ionosphere is described; it occurs on about 60 per cent of the local winter nights in each hemisphere in years of solar minimum activity, and less frequently at other times. During the event the F-region moves downward into the region of rapid recombination and most of its ionization may be lost; a portion of it sometimes enters the E-region to form a pre-sunrise E- or sporadic E-layer. Spaced antenna measurements of F-region horizontal motions during these events are interpreted to support the view that the downward motion is driven by neutral air winds in the F-region, rather than by electrostatic fields.

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