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The sporadic E layer at Kodaikanal

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dc.contributor.author Rangarajan, S
dc.date.accessioned 2010-03-11T16:45:38Z
dc.date.available 2010-03-11T16:45:38Z
dc.date.issued 1954-06
dc.identifier.citation Journal of Geophysical Research, Vol. 59, No. 2, pp. 239 - 246 en
dc.identifier.issn 0148-0227
dc.identifier.uri http://hdl.handle.net/2248/5072
dc.description Open Access en
dc.description.abstract An 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.iso en en
dc.publisher American Geophysical Union en
dc.relation.uri http://www.agu.org/pubs/crossref/1954/JZ059i002p00239.shtml en
dc.rights © American Geophysical Union en
dc.subject Ionospheric Records en
dc.subject Geomagnetic Equator en
dc.subject Sporadic E Layer en
dc.subject Meteoric Activity en
dc.subject Geomagnetic Field en
dc.title The sporadic E layer at Kodaikanal en
dc.type Article en


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