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dc.contributor.authorChakrabarti, N.
dc.contributor.authorLakhina, G.S.
dc.date.accessioned2015-08-20T05:55:14Z
dc.date.accessioned2021-02-12T10:30:06Z-
dc.date.available2015-08-20T05:55:14Z
dc.date.available2021-02-12T10:30:06Z-
dc.date.issued2003
dc.identifier.citationAnnales Geophysicae, v.21, p.1153-1157, 2003, doi: 10.5194/angeo-21-1153-2003en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/242-
dc.description.abstractCollisional Rayleigh-Taylor (RT) instability is considered in the bottom side of the equatorial F-region. By a novel nonmodal calculation it is shown that for an applied shear flow in equilibrium, the growth of the instability is considerably reduced. Finite but small amounts of diffusion enhances the stabilization process. The results may be relevant to the observations of long-lived irregularities at the bottom-side of the F-layer.en_US
dc.language.isoenen_US
dc.subjectIonosphereen_US
dc.subjectIonospheric irregularitiesen_US
dc.subjectEquatorial ionosphereen_US
dc.subjectPlasma wavesen_US
dc.subjectEquatorial F regionen_US
dc.subjectF-layeren_US
dc.titleCollisional Rayleigh-Taylor instability and shear-flow in equatorial Spread-F plasmaen_US
dc.typeArticleen_US
dc.identifier.accession090728
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