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Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/4564
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dc.contributor.authorDeshpande, M. R-
dc.contributor.authorRastogi, R. G-
dc.contributor.authorVats, H. O-
dc.contributor.authorSethia, G-
dc.contributor.authorKlobuchar, J. A-
dc.contributor.authorJain, A. R-
dc.contributor.authorSubbarao, B. S-
dc.contributor.authorPatwari, V. M-
dc.contributor.authorJanve, A. V-
dc.contributor.authorRai, R. K-
dc.contributor.authorSingh, M-
dc.contributor.authorGurm, H. S-
dc.contributor.authorMurthy, B. S-
dc.date.accessioned2009-06-22T15:04:05Z-
dc.date.available2009-06-22T15:04:05Z-
dc.date.issued1977-06-
dc.identifier.citationNature, Vol. 267, pp. 599 - 600en
dc.identifier.issn0028-0836-
dc.identifier.urihttp://hdl.handle.net/2248/4564-
dc.description.abstractThe radio beacon method of measuring TEC along a chain of optimally spaced stations near the equatorial anomaly has been used to monitor continuously the latitudinal extent of the anomaly. Comparisons with the magnitude of the electrojet show a clear dependence of anomaly strength upon the electrojet intensity with an approximate two-hour time delay.en
dc.language.isoenen
dc.publisherNature Publishing Groupen
dc.relation.urihttp://www.nature.com/nature/journal/v267/n5612/abs/267599a0.htmlen
dc.rights© Nature Publishing Groupen
dc.subjectTECen
dc.subjectRadio Beacon Methoden
dc.subjectEffect of Electrojeten
dc.subjectTotal Electron Contenten
dc.subjectThe Indian Subcontinenten
dc.subjectThe Ionosphereen
dc.titleEffect of electrojet on the total electron content of the ionosphere over the Indian subcontinenten
dc.typeArticleen
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