The formation of sporadic E layers by a vortical perturbation excited in a horizontal wind shear flow

The formation of the mid-latitude sporadic E layers (<I>E<sub>s</sub></I> layers) by an atmospheric vortical perturbation excited in a horizontal shear flow (horizontal wind with a horizontal linear shear) is investigated. A three-dimensional atmospheric vortical perturbat...

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Bibliographic Details
Main Authors: G. G. Didebulidze, L. N. Lomidze
Format: Article
Language:English
Published: Copernicus Publications 2008-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/1741/2008/angeo-26-1741-2008.pdf