Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/4530
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dc.contributor.authorChatterjee, Achintya K-
dc.contributor.authorBari, Washimul-
dc.contributor.authorChoudhury, Asit K-
dc.date.accessioned2009-06-09T09:05:20Z-
dc.date.available2009-06-09T09:05:20Z-
dc.date.issued2009-06-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/4530-
dc.description138-142en_US
dc.description.abstractThe very low frequency (VLF) data for over three months (May to July 2008) using Gyrator II loop antenna has been analyzed in the present study. The significant anomalies of D-layer formation time of the ionosphere are observed during sunrise. These anomalies are observed only before, during and after the earthquakes, which took place in the neighboring region. The anomalies were also observed in sunrise terminator time during seismically active days. These abnormal behavior may be due to the lithosphere - ionosphere coupling. These anomalies may be a precursor of earthquake.en_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.relation.ispartof94.20.-y; 95.85.Bh; 94.20.de; 94.20.Vv; 91.30.Pxen_US
dc.sourceIJRSP Vol.38(3) [June 2009]en_US
dc.subjectRadio wave propagationen_US
dc.subjectD-layeren_US
dc.subjectIonospheric disturbancesen_US
dc.subjectEarthquakeen_US
dc.titleAnomalous behavior of D-layer formation time of the ionosphere due to earthquakeen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.38(3) [June 2009]

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