Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/973
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dc.contributor.authorSankaran, K. S-
dc.date.accessioned2006-04-19T05:28:45Z-
dc.date.available2006-04-19T05:28:45Z-
dc.date.issued1964-
dc.identifier.citationThe Indian Journal of Meteorology and Geophysics, Vol. 15, No. 1, pp. 75-82en
dc.identifier.urihttp://hdl.handle.net/2248/973-
dc.description.abstractA special study of cusps and distortions in Fl-layers traces has been made from ionograms obtained at Kodaikanal during a period of about half a solar cycle. Two differnet types of disturbance have been noticed. The first one is a stationary type occuring near the low frequency end of the Fl-layer trace. It is suggested that these ridges found in the course of a disturbance are connected with the E2-layer. In the second type, the cusp appears to move along the virtual height curve and these are ascribed to travelling wave-type disturbance. It is also found that these disturbances are associated with the disappearence. It is also found that these disturbances are associated with the disappearance of equatorial E/subs/ on magnetically disturbed days. An explanation of the phenomenon is attempted in terms of internal gravity waves proposed by Hines (1960)en
dc.format.extent2972329 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoenen
dc.publisherIndian Meteorological Departmenten
dc.subjectIonospheric Fl-layeren
dc.titleCusps and Distortions in Ionospheric Fl-layer observed over Kodaikanalen
dc.typeArticleen
Appears in Collections:IIAP Publications

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