Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456789/704
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dc.contributor.authorMaurya, A.K.
dc.contributor.authorSingh, Rajesh
dc.contributor.authorVeenadhari, B.
dc.contributor.authorKumar, S.
dc.contributor.authorSingh, A.K.
dc.date.accessioned2015-11-26T10:59:26Z
dc.date.accessioned2021-02-12T09:21:09Z-
dc.date.available2015-11-26T10:59:26Z
dc.date.available2021-02-12T09:21:09Z-
dc.date.issued2013
dc.identifier.citationNat. Hazards Earth Syst. Sci., v.13, p.2331-2336, 2013, doi: doi:10.5194/nhess-13-2331-2013en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/704-
dc.description.abstractThe present study reports the VLF (very low frequency) sub-ionospheric perturbations observed on transmitter JJI (22.1 kHz), Japan, received at the Indian low-latitude station, Allahabad ( geographic lat. 25.41° N, long 81.93° E), due to Wenchuan earthquake (EQ) that occurred on 12 May 2008 with the magnitude 7.9 and at the depth of 19 km in Sichuan province of Southwest China, located at 31.0° N, 103.4° E. The nighttime amplitude fluctuation analysis gives a significant increase in fluctuation and dispersion two days before EQ, when it crosses 2σ criterion. However, there was no significant change observed in the amplitude trend. The diurnal amplitude variation shows a significant increase in the amplitude of JJI signal on 11 and 12 May 2008. The gravity wave channel and changes in the electric field associated with this EQ seem to be the potential factors of the observed nighttime amplitude fluctuation, dispersion, and significant increase in the signal strength.en_US
dc.language.isoenen_US
dc.subjectVery low frequencyen_US
dc.subjectWenchuan earthquakeen_US
dc.subject12 May 2008en_US
dc.subjectVLFen_US
dc.subjectEQen_US
dc.titleSub-ionospheric very low frequency perturbations associated with the 12 May 2008 M = 7.9 Wenchuan earthquakeen_US
dc.typeArticleen_US
dc.identifier.accession091365
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