The influence of atmospheric gravity waves evolving in horizontal shear flow on the ionosphere F2-layer

The ionosphere F2-layer height profile of the electron density is obtained by using the presence of atmospheric gravity waves (GW) evolving in horizontal shear flow. The possible responsibility of the GW evolving in the horizontal shear flow for the formation of large scale travelling ionospheric di...

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Bibliographic Details
Published inPhysics letters. A Vol. 252; no. 6; pp. 328 - 335
Main Authors Didebulidze, G.G., Pataraya, A.D.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 08.03.1999
Subjects
Atmospheric gravity waves
Ionosphere
Atmospheric gravity waves
Ionosphere
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Summary:The ionosphere F2-layer height profile of the electron density is obtained by using the presence of atmospheric gravity waves (GW) evolving in horizontal shear flow. The possible responsibility of the GW evolving in the horizontal shear flow for the formation of large scale travelling ionospheric disturbance (TID) with small periods is shown.
ISSN:0375-9601
1873-2429
DOI:10.1016/S0375-9601(98)00951-7