Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/3824
Full metadata record
DC FieldValueLanguage
dc.contributor.authorSastri, J. H-
dc.date.accessioned2008-09-23T13:47:19Z-
dc.date.available2008-09-23T13:47:19Z-
dc.date.issued1984-06-
dc.identifier.citationAnnales Geophysicae, Vol. 2, No. 3, pp. 353 - 358en
dc.identifier.issn0755-0685-
dc.identifier.urihttp://hdl.handle.net/2248/3824-
dc.descriptionOpen Access-
dc.description.abstractFrom an analysis of ionogram data of Kodaikanal (dip 3.5 deg N) for a 3-yr period of high sunspot activity, it is shown that the duration of equatorial spread-F (ESF), on the average, bears a direct relationship to the peak amplitude as well as duration of the post-sunset enhancement in F-region upward vertical drift in all seasons. The duration of ESF is also found to exhibit a significant positive correlation with the altitude of bottomside F-region at the time of onset of ESF but only during equinoxes and northern winter (D) months.en
dc.language.isoenen
dc.publisherCopernicus Publicationsen
dc.relation.urihttp://www.ann-geophys.net/volumes_and_issues.htmlen
dc.rights© European Geosciences Union-
dc.subjectIonogram Dataen
dc.subjectEquatorial Spread-Fen
dc.subjectSunspot Activityen
dc.titleDuration of equatorial spread-Fen
dc.typeArticleen
Appears in Collections:IIAP Publications

Files in This Item:
File Description SizeFormat 
Duration of equatorial spread-F.pdfOpen Access304.24 kBAdobe PDFThumbnail
View/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.