2010 Leh floods
   HOME

TheInfoList



OR:

The 2010 Ladakh floods occurred on 6 August 2010 across a large part of
Ladakh Ladakh () is a region administered by India as a union territory which constitutes a part of the larger Kashmir region and has been the subject of dispute between India, Pakistan, and China since 1947. (subscription required) Quote: "Jammu ...
, then part of the state of Jammu and Kashmir. 71 towns and villages were damaged, including the main town in the area,
Leh Leh () ( lbj, ) is the joint capital and largest city of Ladakh, a union territory of India. Leh, located in the Leh district, was also the historical capital of the Kingdom of Ladakh, the seat of which was in the Leh Palace, the former res ...
.Hobley, D.E.J., et al., 2012, Reconstruction of a major storm event from its geomorphic signature: The Ladakh floods, 6 August 2010, Geology, v. 40, p. 483-486, doi:10.1130/G32935.1 At least 255 people are reported to have died, six of whom were foreign tourists, after a
cloudburst A cloudburst is an extreme amount of precipitation in a short period of time, sometimes accompanied by hail and thunder, which is capable of creating flood conditions. Cloudbursts can quickly dump large amounts of water, e.g. 25 mm of pre ...
and heavy overnight rains triggered flash floods,
mudflow A mudflow or mud flow is a form of mass wasting involving fast-moving flow of debris that has become liquified by the addition of water. Such flows can move at speeds ranging from 3 meters/minute to 5 meters/second. Mudflows contain a significa ...
s, and
debris flow Debris flows are geological phenomena in which water-laden masses of soil and fragmented rock rush down mountainsides, funnel into stream channels, entrain objects in their paths, and form thick, muddy deposits on valley floors. They generally ...
s. 200 people were reported missing in the initial aftermath of the storm, and thousands more were rendered homeless after the flooding caused extensive damage to property and infrastructure. Overall, 9000 people were directly affected by the event.


History

Leh Leh () ( lbj, ) is the joint capital and largest city of Ladakh, a union territory of India. Leh, located in the Leh district, was also the historical capital of the Kingdom of Ladakh, the seat of which was in the Leh Palace, the former res ...
is the largest town in the
Ladakh Ladakh () is a region administered by India as a union territory which constitutes a part of the larger Kashmir region and has been the subject of dispute between India, Pakistan, and China since 1947. (subscription required) Quote: "Jammu ...
region of the Indian state of Jammu and Kashmir. It is on a plateau at around above sea level and usually receives very little rainfall, around per year. Described as a " high-altitude cold desert", the area has sparse rainfall and a heavy downpour is a rare occurrence. The average rainfall in Leh for the month of August is , with highest rainfall ever recorded during a single 24-hour period being , recorded on 22 August 1933. The town is predominantly Buddhist. Tourists are attracted by its natural environment. August is the peak tourist season when thousands of western backpackers come to the area. Leh receives about 60,000 foreign and 150,000 domestic tourists annually.


Flooding and damage

The flash floods happened after a night of heavy downpour. The cloudburst itself occurred between 0000–0030 hours IST on 6 August 2010, leading to flash flooding,
debris flows Debris flows are geological phenomena in which water-laden masses of soil and fragmented rock rush down mountainsides, funnel into stream channels, entrain objects in their paths, and form thick, muddy deposits on valley floors. They generall ...
, and
mudflow A mudflow or mud flow is a form of mass wasting involving fast-moving flow of debris that has become liquified by the addition of water. Such flows can move at speeds ranging from 3 meters/minute to 5 meters/second. Mudflows contain a significa ...
s over the region. The rainfall distribution was highly spatially variable. The most intense part of the storm was focused in a -wide band parallel to, and a few kilometers from, the river Indus. This band was centred over most of the major settlements in the area, including Leh. Outside the band, the rainfall intensity was unremarkable; the only weather station in the area, at Leh airport, recorded just of total rainfall for the night of 6 August. However, within it precipitation intensities were over an order of magnitude higher, peaking at at least over Leh during the most intense part of the storm. Estimates of the maximum total rainfall in some places were as high as . Note that the implied of rain over Leh during the most intense part of the storm is equivalent to around a year's worth of rain falling in 30 minutes. The rains occurred at night, and surprised everyone. In Leh, many buildings were destroyed including hospitals, the bus terminal, radio station transmitter, telephone exchange and mobile-phone towers. BSNL communication systems were fully destroyed. Communications were later restored by the Indian Army. The local bus station was severely damaged and some of the buses were carried more than a mile by the mud. The city's airport was damaged but was rapidly repaired to allow relief flights the following day. The village of Choglamsar on the outskirts of the city was particularly badly hit. In neighbouring valleys, large numbers of smaller villages which lay under the main rainfall band were also heavily damaged, with large numbers of casualties. As in Leh, much of the destruction was caused by debris flows coming from the rocky sidewalls of the valleys, not by the flooding itself. Notable impacts occurred in Sobu, Phyang, Nimu, Nyeh, and Basgo villages. In total, almost 1500 homes in 71 settlements across the area were reported to have been damaged. Detailed mapping and estimation of the entrapped sediment mass within the transverse stream valleys of various sectors of Himalaya is required to predict the style of mass transfer during such events."Sedimentary and Geomorphic Signatures of a Cloud burst and triggered flash floods in the Indus valley of Ladakh Himalaya". SSG S.J. Sangode, D.C. Meshram, S. Rawat, Y. Kulkarni, D.M. Chate. Himalayan Geology 38 (1), 12-29. All of the estimated 3000 tourists in Leh, including 1000 foreigners were safe according to local officials. Outside the town, six tourists were reported killed. However, official documents indicate that at least 255 local residents were killed, with a further 29 never found. The true toll may have been significantly higher, perhaps more than 600 people.


Response

The rescue efforts were hampered by gushing water and mud which was 10 feet high in places. In addition many of the roads and bridges leading to Leh were damaged, making it difficult to truck in relief supplies. Four hundred critically wounded people were evacuated and some were admitted to the army hospital in Leh.
Indian Army The Indian Army is the land-based branch and the largest component of the Indian Armed Forces. The President of India is the Supreme Commander of the Indian Army, and its professional head is the Chief of Army Staff (COAS), who is a four- ...
soldiers launched a massive rescue operation. Home minister P. Chidambaram said that over 6,000 security personnel were deployed in Leh for rescue operations. Prime minister Manmohan Singh expressed grief and announced compensation of Rs. 100,000 to the kin of deceased and Rs. 50,000 for those injured. Chief Minister of the state
Omar Abdullah Omar Abdullah (; born 10 March 1970) is an Indian politician and former Chief Minister of the erstwhile state of Jammu and Kashmir. He became the 11th and the youngest Chief Minister of the State of Jammu and Kashmir, after forming a governme ...
directed the administration to undertake relief effort on a war footing.


See also

*
Ladakh Marathon The Ladakh Marathon is a marathon held in Leh, a town in the Indian Union Territory of Ladakh. It claims to be the highest marathon in the world, held at a height of . The seventh edition of the Ladakh Marathon was held in 2018 and its ninth ed ...
* Global storm activity of 2010 * 2008 South China floods *
2010 Pakistan floods The floods in Pakistan began in late July 2010, resulting from heavy monsoon rains in the Khyber Pakhtunkhwa, Sindh, Punjab and, Balochistan regions of Pakistan, which affected the Indus River basin. Approximately one-fifth of Pakistan's tot ...
*
2010 China floods The 2010 China floods began in early May 2010.. Three hundred and ninety-two people died, and a further 232 people were reported missing as of June 30, 2010, including 57 people in a landslide in Guizhou. Fifty-three of the deaths occurred from t ...
*
Monsoon A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal osci ...


References


External links


Leh , The Post-Flood Report ( December 2010)
@ vistet.wordpress
Video:Leh floods: Omar visits hospital, meets victims
NDTV
Video:Ladakh: Rebuilding lives
NDTV

CNN-IBN
Leh Flash Floods 2010
at WN
CDRN Response for Flash Floods Relief Work in Leh, Jammu & Kashmir
India Corporate Disaster Resource Network (https://web.archive.org/web/20121105042435/http://www.cdrn.org.in/)
Marka valley & Leh & Choglamsar
Film of the torrential mud {{Buddhist monasteries in Ladakh Leh Floods, 2010 Leh Floods, 2010 Floods in India Ladakh floods 2010 2010s in Jammu and Kashmir Disasters in Jammu and Kashmir History of Ladakh Ladakh floods