On the possibility of in situ shear excitation of vortical perturbations and their coupling with short-period gravity waves by airglow and ionosphere observations-Reference-Cited by-同舟云学术

On the possibility of in situ shear excitation of vortical perturbations and their coupling with short-period gravity waves by airglow and ionosphere observations

Published:2002-05 Issue:8-11 Volume:64 Page:1105-1116
ISSN:1364-6826
Container-title:Journal of Atmospheric and Solar-Terrestrial Physics
language:en
Short-container-title:Journal of Atmospheric and Solar-Terrestrial Physics

Author:

Didebulidze G.G,Chilingarashvili S.P,Toroshelidze T.I,Murusidze I.G,Kvavadze N.D,Sharadze Z.S

Publisher

Elsevier BV

Subject

Space and Planetary Science,Atmospheric Science,Geophysics

Reference36 articles.

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3. Amplification/damping processes of atmospheric acoustic-gravity waves in horizontal winds with linear shear;Didebulidze;Physics Letters A,1997

4. Evolution of atmospheric gravity waves in horizontal shear flow;Didebulidze;Physica Scripta,1999

5. Ionosphere F2-region under the influence of the evolutional atmospheric gravity waves in horizontal shear flow;Didebulidze;Journal of Atmospheric and Solar-Terrestrial Physics,1999

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1. Cosmic factors influence on the inter-annual variations of the green 557.7 Nm line and red 630.0 Nm line nightglow intensities and their possible coupling with cloud covering at Abastumani (41.75°N, 42.82°E);Acta Geophysica;2013-04-19

2. Long-term changes in the nightly behaviour of the oxygen red 630.0 nm line nightglow intensity and trends in the thermospheric meridional wind velocity;International Journal of Remote Sensing;2011-06-10

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4. Multilayered structures in the ionosphereF2region and impulse-like increase of the nightglow red 630 nm line intensity as a result of influence of shear excited atmospheric vortical perturbations;Journal of Geophysical Research: Space Physics;2009-03

5. Different long-term trends of the oxygen red 630.0 nm line nightglow intensity as the result of lowering the ionosphere F2 layer;Annales Geophysicae;2008-07-31