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Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/4635
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dc.contributor.authorDas Gupta, A-
dc.contributor.authorBasu, S-
dc.contributor.authorBhar, J. N-
dc.contributor.authorBhattacharyya, J. C-
dc.date.accessioned2009-07-14T11:54:26Z-
dc.date.available2009-07-14T11:54:26Z-
dc.date.issued1975-02-
dc.identifier.citationJournal of Geophysical Research, Vol. 80, pp. 699 - 701en
dc.identifier.issn0148-0227-
dc.identifier.urihttp://hdl.handle.net/2248/4635-
dc.description.abstractThe ionospheric total electron content and equivalent slab thickness in the equatorial region around 75° E have been studied. It is found that the slab thickness exhibits a strong latitudinal dependence with a maximum at the magnetic equator and a minimum around the crest of the F/sub2 anomaly, indicating that the F region is thick near the equator and most skewed near the crest. The results are consistent with the electrodynamic drift and diffusion in the equatorial ionosphere.en
dc.language.isoenen
dc.publisherAmerican Geophysical Unionen
dc.relation.urihttp://adsabs.harvard.edu/abs/1975JGR....80..699Den
dc.subjectDiurnal Variationsen
dc.subjectF Regionen
dc.subjectIonospheric Driften
dc.subjectIonospheric Electron Densityen
dc.subjectMagnetic Equatoren
dc.subjectPlasma Slabsen
dc.subjectAbnormalitiesen
dc.subjectAtmospheric Diffusionen
dc.subjectPlasma Diffusionen
dc.subjectTropical Regionsen
dc.subjectWinteren
dc.titleIonospheric electron content and equivalent slab thickness in the equatorial regionen
dc.typeArticleen
Appears in Collections:IIAP Publications
J.C.Bhattacharyya (1982 - 1990)

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