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dc.contributor.authorSingh, Darshan-
dc.contributor.authorSingh, Manjit-
dc.date.accessioned2014-01-15T06:12:50Z-
dc.date.available2014-01-15T06:12:50Z-
dc.date.issued2005-10-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25667-
dc.description328-331en_US
dc.description.abstractThe western disturbances affect the mesosphere/lower thermosphere such that low frequency propagation field strength exhibits fadings/scintillations. The degree of effect depend, upon the severity of disturbance. Periodic variations are due to internal atmospheric gravity waves and scintillations are due to irregularities produced by thundercloud activity. The study represents magnitude of electrostatic coupling between the troposphere and ionosphere.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.relation.ispartof92.60.Nv; 92.60. Ta; 94.20. Yxen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.34(5) [October 2005]en_US
dc.subjectWestern disturbancesen_US
dc.subjectThundercloudsen_US
dc.subjectFadingsen_US
dc.subjectScintillationsen_US
dc.titleEffect of western disturbances on LF 164 kHz propagationen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.34(5) [October 2005]

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