Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/5072
Full metadata record
DC FieldValueLanguage
dc.contributor.authorRangarajan, S-
dc.date.accessioned2010-03-11T16:45:38Z-
dc.date.available2010-03-11T16:45:38Z-
dc.date.issued1954-06-
dc.identifier.citationJournal of Geophysical Research, Vol. 59, No. 2, pp. 239 - 246en
dc.identifier.issn0148-0227-
dc.identifier.urihttp://hdl.handle.net/2248/5072-
dc.descriptionOpen Accessen
dc.description.abstractAn examination of the ionospheric records at Kodaikanal, which is located almost on the geomagnetic equator, reveals that the sporadic E layer here has some regular features not observed at other latitudes. It occurs in nearly 93 per cent of the half-hourly records during the daytime. Two main types of Es are observed; namely, (1) the patchy type with a well-marked diurnal variation, and (2) the blanketing type which occurs mostly during afternoons. It is found that neither meteoric activity nor thunderstorm activity has any appreciable influence on the formation of either of the two types of Es. No correlation is observed between Es and the geomagnetic field.en
dc.language.isoenen
dc.publisherAmerican Geophysical Unionen
dc.relation.urihttp://www.agu.org/pubs/crossref/1954/JZ059i002p00239.shtmlen
dc.rights© American Geophysical Unionen
dc.subjectIonospheric Recordsen
dc.subjectGeomagnetic Equatoren
dc.subjectSporadic E Layeren
dc.subjectMeteoric Activityen
dc.subjectGeomagnetic Fielden
dc.titleThe sporadic E layer at Kodaikanalen
dc.typeArticleen
Appears in Collections:IIAP Publications

Files in This Item:
File Description SizeFormat 
The sporadic E layer at Kodaikanal224.01 kBAdobe PDFThumbnail
View/Open


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