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dc.contributor.authorSingh, Rajesh
dc.contributor.authorSiingh, Devendraa
dc.contributor.authorGokani, Sneha A.
dc.contributor.authorBuchunde, P.S.
dc.contributor.authorSingh, R.P.
dc.contributor.authorSingh, A.K.
dc.date.accessioned2015-12-14T11:24:36Z
dc.date.accessioned2021-02-12T09:21:24Z-
dc.date.available2015-12-14T11:24:36Z
dc.date.available2021-02-12T09:21:24Z-
dc.date.issued2015
dc.identifier.citationNat. Hazards Earth Syst. Sci. Discuss., v.3, p.941-953, 2015, doi: 10.5194/nhessd-3-941-2015en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/826-
dc.description.abstractThe devastating episode (17–18 June 2013) at Kedarnath (Uttrakhand, India) caused huge loss of lives and physical/material wealth. To understand this catastrophic event, rainfall/convective data and associated climate meteorological parameters are investigated. Low pressure zone with very high cloud cover (60–90%), and relative humidity (70–100%) associated with low (< 4 m s−1) wind velocity over Kedarnath region during 15–17 June are observed. The cause of disaster seems to be the heavy and continuous rainfall associated with snow melting and over flooding/collapse of the Chorabari Lake, located upstream. Monsoon advancement was much faster due to the presence of convectively active phase of the Madden Julian Oscillation.en_US
dc.language.isoenen_US
dc.subjectClimateen_US
dc.subjectTopographicalen_US
dc.subjectMeteorologicalen_US
dc.subjectDisaster causesen_US
dc.subjectKedarnathen_US
dc.subjectMonsoonen_US
dc.titleBrief Communication: Climate, topographical and meteorological investigation of the 16-17 June 2013 Kedarnath (India) disaster causesen_US
dc.typeArticleen_US
dc.identifier.accession091490
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