Authors: Wagnon, Patrick; Linda, Anurag; Arnaud, Yves; Kumar, Rajesh; Sharma, Parmanand; Vincent, Christian; Pottakkal, Jose George; Berthier, Etienne; Ramanathan, Alagappan; Hasnain, Syed Iqbal; Chevallier, Pierre

Source: Journal of Glaciology, Volume 53, Number 183, December 2007 , pp. 603-611(9)

Publisher: International Glaciological Society

Abstract:

Little is known about the Himalayan glaciers, although they are of particular interest in terms of future water supply, regional climate change and sea-level rise. In 2002, a long-term monitoring programme was started on Chhota Shigri Glacier (32.2°N, 77.5°E; 15.7 km², 6263-4050 m a.s.l., 9 km long) located in Lahaul and Spiti Valley, Himachal Pradesh, India. This glacier lies in the monsoon-arid transition zone (western Himalaya) which is alternately influenced by Asian monsoon in summer and the mid-latitude westerlies in winter. Here we present the results of a 4 year study of mass balance and surface velocity. Overall specific mass balances are mostly negative during the study period and vary from a minimum value of -1.4 m w.e. in 2002/03 and 2005/06 (equilibrium-line altitude (ELA) ∼5180 m a.s.l.) to a maximum value of +0.1 m w.e. in 2004/05 (ELA 4855 m a.s.l.). Chhota Shigri Glacier seems similar to mid-latitude glaciers, with an ablation season limited to the summer months and a mean vertical gradient of mass balance in the ablation zone (debris-free part) of 0.7 m w.e. (100 m)^-1, similar to those reported in the Alps. Mass balance is strongly dependent on debris cover, exposure and the shading effect of surrounding steep slopes.

Document Type: Research article

DOI: http://dx.doi.org/10.3189/002214307784409306

Publication date: 2007-12-01

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