dc.contributor.author |
Singh, Rajesh |
|
dc.contributor.author |
Siingh, Devendraa |
|
dc.contributor.author |
Gokani, Sneha A. |
|
dc.contributor.author |
Buchunde, P.S. |
|
dc.contributor.author |
Singh, R.P. |
|
dc.contributor.author |
Singh, A.K. |
|
dc.date.accessioned |
2015-12-14T11:24:36Z |
|
dc.date.accessioned |
2021-02-12T09:21:24Z |
|
dc.date.available |
2015-12-14T11:24:36Z |
|
dc.date.available |
2021-02-12T09:21:24Z |
|
dc.date.issued |
2015 |
|
dc.identifier.citation |
Nat. Hazards Earth Syst. Sci. Discuss., v.3, p.941-953, 2015, doi: 10.5194/nhessd-3-941-2015 |
en_US |
dc.identifier.uri |
http://localhost:8080/xmlui/handle/123456789/826 |
|
dc.description.abstract |
The 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.iso |
en |
en_US |
dc.subject |
Climate |
en_US |
dc.subject |
Topographical |
en_US |
dc.subject |
Meteorological |
en_US |
dc.subject |
Disaster causes |
en_US |
dc.subject |
Kedarnath |
en_US |
dc.subject |
Monsoon |
en_US |
dc.title |
Brief Communication: Climate, topographical and meteorological investigation of the 16-17 June 2013 Kedarnath (India) disaster causes |
en_US |
dc.type |
Article |
en_US |
dc.identifier.accession |
091490 |
|