The devastating flood episode (16-17 June 2013) at Kedarnath (Uttrakhand, India), caused a huge loss of lives and loss of physical/material wealth. To understand this catastrophic event, rainfall/convective data and associated climate meteorological parameters are investigated. A low-pressure zone with very high cloud cover (60-90 %) and relative humidity (70-100 %), associated with low (< 4 m s -1) wind velocity, are observed over the Kedarnath region during 15-17 June. The cause of this disaster seems to be heavy and continuous rainfall, associated with snowmelt and the overflooding/collapse of Chorabari Lake, located upstream. Monsoon advancement was much faster than usual, due to the presence of the convectively active phase of the Madden-Julian oscillation.
CITATION STYLE
Singh, R., Siingh, D., Gokani, S. A., Sreeush, M. G., Buchunde, P. S., Maurya, A. K., … Singh, A. K. (2015). Brief Communication: Climatic, meteorological and topographical causes of the 16-17 June 2013 Kedarnath (India) natural disaster event. Natural Hazards and Earth System Sciences, 15(7), 1597–1601. https://doi.org/10.5194/nhess-15-1597-2015
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