Cause of deadly 2010 Himachal flood revealed
Researchers have found the root cause of the flash flood that hit Leh on the night of Aug. 5, 2010, causing severe damage and leaving 193 dead, hundreds missing and thousands homeless.
Washington: Researchers have found the root cause of the flash flood that hit Leh, an Indian town in a high desert valley in the Himalayas, on the night of Aug. 5, 2010, causing severe damage and leaving 193 dead, hundreds missing and thousands homeless.
The have concluded that the deadly flood was set off by a string of unusual weather events not unlike those that caused devastating flash floods in Colorado and South Dakota in the 1970s.
“Flash flooding events don’t happen often but when they do they are some of the scariest, most dangerous and quickest natural disasters that can happen,” said Kristen Rasmussen, a University of Washington graduate student in atmospheric sciences.
“But now that we know what types of conditions to look out for, flash flood warnings in remote regions of India might be possible,” she stated.
Rasmussen and Robert Houze, a UW professor in atmospheric sciences, studied satellite images and what’s called re-analysis data to piece together what happened to create such a torrential downpour.
They found that on three consecutive days clouds formed high in the mountains to the east over the Tibetan Plateau. By itself, that isn’t uncommon, Rasmussen said.
“What’s different in this case is that there was the unusual wind coming from the east and blowing west,” she said.
That helped the clouds clump together and build into a larger storm system capable of creating heavy rain over Leh, which is 11,480 feet above sea level.
At the same time, low-level winds carried in moisture from both the Bay of Bengal and the Arabian Sea.
“The storm, forming just up the slope, was able to tap into that additional moisture,” she said.
Typically, such large storm systems don’t have the chance to build because each day as the sun sets, the warm air that has helped the clouds form and lift gets cooler. The clouds then die out in the evening. But during those three days of August 2010, the unusual wind blew through the night, spurring the clouds to continue building into a system capable of heavy rain.
The storm, formed when unusual winds from the east organized clouds that had formed high in the mountains, tapped into moisture from both the Bay of Bengal and the Arabian Sea.
Above-average rain fell on the first two days. Since the region typically gets so little rainfall, the soil doesn’t absorb water well.
“The key is that this happened for three successive days. If the third day hadn’t happened or if the first two days hadn’t set the process in motion, there probably wouldn’t have been such a devastating flash flood,” Rasmussen said.
The situation is reminiscent of weather that caused deadly flooding through the Big Thompson Canyon in Colorado in 1976 and the Black Hills of South Dakota in 1972. In all three cases, large organized clouds gathered high in the mountains and drew moisture up the slope of the mountain into the storms.
Now that researchers have identified these common elements, including organized clouds high in the mountains on the edge of an arid plain with unusual access to moisture, weather forecasters can potentially warn people who could be in danger if a flash flood happens, Rasmussen said.
The research appeared in the Nov. 14 Bulletin of the American Meteorological Society.