| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1776348 | Journal of Atmospheric and Solar-Terrestrial Physics | 2015 | 11 Pages |
Abstract
The Es layers mainly move downwards, but at certain spatial location, where temporal changes in wave phase caused by background shear flow and AGW are small, these layers are almost horizontal. The vertical spatial location of the horizontal Es layers is determined by the vertical wavelength of atmospheric gravity waves.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
G.G. Didebulidze, G. Dalakishvili, L. Lomidze, G. Matiashvili,