Coupling effect of the equatorial F region irregularities on the low latitude E region instability processes

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dc.contributor.author Patra, A.K.
dc.contributor.author Sripathi, S.
dc.contributor.author Tiwari, D.
dc.date.accessioned 2015-08-28T09:30:04Z
dc.date.accessioned 2021-02-12T10:30:29Z
dc.date.available 2015-08-28T09:30:04Z
dc.date.available 2021-02-12T10:30:29Z
dc.date.issued 2004
dc.identifier.citation Geophysical Research Letters, v.31/17, 2004, doi: 10.1029/2004GL020486 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/299
dc.description.abstract [1] Simultaneous observations of E and F region irregularities made using the Gadanki MST radar are presented. The observations show that the E region echoes weaken or disappear during the growth phase of the topside F region irregularities. Unlike Jicamarca observations, no valley region echoes are observed during this phase. It is shown that the weakening or disappearance of E region signals are not directly coupled with the F region irregularities just overhead, but linked with the instability processes over the magnetic equator through the magnetic field lines. It is proposed that the fringe fields present in the valley region in association with the equatorial F region plasma bubbles, in the presence of appropriate background electric field conditions, are responsible candidates. It is shown that these fringe fields and the electric fields associated with the irregularities in the valley region can map to the low latitude E region and thereby inhibit the growth of the E region instability processes as revealed by the Gadanki radar observations. en_US
dc.language.iso en en_US
dc.subject F region irregularitie en_US
dc.subject E region irregularitie en_US
dc.subject Electric fields en_US
dc.subject Gadanki radar observations en_US
dc.title Coupling effect of the equatorial F region irregularities on the low latitude E region instability processes en_US
dc.type Article en_US
dc.identifier.accession 090789


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