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We describe a new, self‐consistent scenario in which sporadic‐ E doublets, height bands of upward‐displaced F ‐layer profiles, F ‐region plasma depletions, and radar backscatter plumes, are all manifestations of a coupled electrodynamical response by the nighttime midlatitude ionosphere to the presence of a traveling ionospheric disturbance (TID). We show that the response consists of (1) formation of image plasma structure in the E region, (2) initiation of a Hall‐current‐driven polarization process by the E ‐region plasma structure, and (3) mapping of the polarization electric field to the F region, where it strengthens the electrical properties of the TID that initiated the E ‐region processes. This scenario provides ready answers for several, hitherto puzzling, questions and a basis for new directions on this research topic.
Tsunoda et al. (Thu,) studied this question.
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