Glacial lake outburst flood risk assessment of Sun Koshi basin, Nepal

The ongoing retreat of glaciers in the Hindu Kush-Himalaya (HKH) is associated with climate change. While deglaciation can cause a suite of impacts, one of the most visible and tangible impacts is the formation of glacial lakes. Some of these lakes can burst out causing large flash floods with the potential to cause significant damage to property, lives and livelihoods. At the moment, knowledge of the current glacial lake outburst flood (GLOF) risk in the HKH is incomplete, and a proper risk assessment is often circumvented. There is a need for a comprehensive GLOF risk assessment in order to support proper planning of mitigation and adaptation strategies in this context. In this paper we present a methodological approach for the GLOF risk assessment. The major part of the risk assessment is GLOF simulation and downstream impact assessment. The methodology was applied to the Sun Koshi river basin, a trans-boundary river basin between Tibet (China) and Nepal. A glacial lake outburst hydrograph was simulated using a dambreak model. The outburst flood was routed along the river using a hydrodynamic model to estimate the potential impact areas. A field survey was conducted to assess the potential damage caused by the GLOF. The peak outburst flood could be in the order of 7900 m3 s−1. The analysis shows that about 950 ha of land and a large amount of infrastructure are exposed to the GLOF. The economic risk due to the direct impact of a GLOF is estimated to be about US$197 million.

[1]  Jiawen Ren,et al.  Glacier variations and climate warming and drying in the central Himalayas , 2004 .

[2]  J. Reynolds DEVELOPMENT AND CLIMATE CHANGE IN NEPAL: FOCUS ON WATER RESOURCES AND HYDROPOWER , 2003 .

[3]  H. L. Miller,et al.  Climate Change 2007: The Physical Science Basis , 2007 .

[4]  Donghui Shangguan,et al.  The retreat of glaciers in response to recent climate warming in western China , 2006, Annals of Glaciology.

[5]  P. Mayewski,et al.  Himalayan and Trans-Himalayan Glacier Fluctuations Since AD 1812 , 1979 .

[6]  S. Solomon The Physical Science Basis : Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change , 2007 .

[7]  S. Yamaguchi,et al.  Shrinkage of the Khumbu Glacier, east Nepal from 1978 to 1995 , 2000 .

[8]  D. R. Gurung,et al.  Inventory of Glaciers, Glacial Lakes and Glacial Lake Outburst Floods: Monitoring and Early Warning Systems in the Hindu Kush-Himalayan Region - Bhutan , 2001 .

[9]  W. Haeberli,et al.  Construction, environmental problems and natural hazards in periglacial mountain belts , 1992 .

[10]  K. Fujita,et al.  Glaciological observations on Rikha Samba Glacier in Hidden Valley, Nepal Himalayas, 1998 and 1999 , 2001 .

[11]  K. Fujita,et al.  Changes in glaciers in Hidden Valley, Mukut Himal, Nepal Himalayas, from 1974 to 1994 , 1997, Journal of Glaciology.

[12]  Gary W. Brunner,et al.  HEC-RAS River Analysis System. Hydraulic Reference Manual. Version 1.0. , 1995 .

[13]  Wanqin Guo,et al.  Assessment and Simulation of Glacier Lake Outburst Floods for Longbasaba and Pida Lakes, China , 2008 .

[14]  T. Kadota On the relation between climate and retreat of Glacier AX010 in the Nepal Himalaya from 1978 to 1989 , 1992 .

[15]  D. L. Fread,et al.  BREACH: An erosion model for earthen dam failures , 1988 .

[16]  A. Shrestha,et al.  Glacial Lake Outburst Floods in the Sagarmatha Region , 2007 .

[17]  A. Shrestha Resource Manual on Flash Flood Risk Management; Module 2: Non-Structural Measures , 2008 .

[18]  John M. Reynolds,et al.  High-altitude glacial lake hazard assessment and mitigation: a Himalayan perspective , 1998, Geological Society, London, Engineering Geology Special Publications.

[19]  A. Shrestha,et al.  Resource Manual on Flash Flood Risk Management , 2012 .