Meteorological conditions, seasonal and annual mass balances of Chhota Shigri Glacier, western Himalaya, India

被引:87
作者
Azam, Mohd Farooq [1 ,2 ,3 ]
Ramanathan, Al [2 ]
Wagnon, P. [1 ,4 ]
Vincent, C. [5 ]
Linda, A. [2 ,6 ]
Berthier, E. [7 ]
Sharma, P. [2 ]
Mandal, A. [2 ]
Angchuk, T. [2 ]
Singh, V. B. [2 ]
Pottakkal, J. G. [2 ,8 ]
机构
[1] UJF Grenoble 1, CNRS, LTHE, IRD,G INP,LGGE,UMR 5183,UMR 5564, F-38402 Grenoble, France
[2] Jawaharlal Nehru Univ, Sch Environm Sci, New Delhi, India
[3] Natl Inst Hydrol, Water Resources Syst Div, Roorkee, Uttar Pradesh, India
[4] Int Ctr Integrated Mt Dev, Kathmandu, Nepal
[5] UJF Grenoble 1, CNRS, LGGE, UMR 5183, F-38041 Grenoble, France
[6] Cent Univ Himachal Pradesh, Sch Earth & Environm Sci, Dept Environm Sci, Dharamshala, India
[7] Univ Toulouse, CNRS, LEGOS, Toulouse, France
[8] Natl Inst Hydrol, Western Himalayan Reg Ctr, Jammu, India
关键词
accumulation; glacier mass balance; glacier meteorology; mountain glaciers; SURFACE-ENERGY BALANCE; CLIMATE-CHANGE; NEPAL HIMALAYA; ALTITUDE; SERIES; ALPS;
D O I
10.3189/2016AoG71A570
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We present the updated glaciological mass balance (MB) of Chhota Shigri Glacier, the longest continuous annual MB record in the Hindu-Kush Karakoram Himalaya (HKH) region. Additionally, 4 years of seasonal MBs are presented and analyzed using the data acquired at an automatic weather station (AWS-M) installed in 2009 on a lateral moraine (4863ma.s.l.). The glaciological MB series since 2002 is first recalculated using an updated glacier hypsometry and then validated against geodetic MB derived from satellite stereo-imagery between 2005 (SPOT5) and 2014 (Pleiades). Chhota Shigri Glacier lost mass between 2002 and 2014 with a cumulative glaciological MB of -6.72 m w. e. corresponding to a mean annual glacier-wide MB (B-a) of -0.56m w. e. a(-1). Equilibriumline altitude (ELA(0)) for the steady-state condition is calculated as similar to 4950 m a.s.l., corresponding to an accumulation-area ratio (AAR(0)) of similar to 61%. Analysis of seasonal MBs between 2009 and 2013 with air temperature from AWS-M and precipitation from the nearest meteorological station at Bhuntar (1050 m a.s.l.) suggests that the summer monsoon is the key season driving the interannual variability of Ba for this glacier. The intensity of summer snowfall events controls the B-a evolution via controlling summer glacier-wide MB (B-s).
引用
收藏
页码:328 / 338
页数:11
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