Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/36165
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dc.contributor.authorDe, S S-
dc.contributor.authorGhosh, B-
dc.contributor.authorMal, Manasi-
dc.contributor.authorGhosh, Bithika-
dc.contributor.authorSarkar, B K-
dc.contributor.authorAdhikari, S K-
dc.date.accessioned2016-10-26T05:11:04Z-
dc.date.available2016-10-26T05:11:04Z-
dc.date.issued1991-04-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36165-
dc.description107-113en_US
dc.description.abstractMaxwell’s equations are solved for the upper atmospheric medium during ionospheric modification enhanced by the propagation of high power radio waves. The form of the solution may be useful for numerical computations to calculate the fields at arbitrary distances from the source. From the governing equations, coupled equations are obtained from which the phenomenon of gradient coupling within the medium may be understood. The variation of normalized electron density with the change of propagation frequency and also the variation of electric field with height during the modified situation have been computed and presented graphically.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.20(2) [April 1991]en_US
dc.titleWave propagation through the upper atmosphere during ionospheric modificationen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.20(2) [April 1991]

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