Estimation of snow/glacier melt contribution in the upper part of the Beas River basin, Himachal Pradesh, using conventional and SNOWMOD modeling approach

被引:11
作者
Ahluwalia, Rajeev Saran [1 ]
Rai, S. P. [2 ]
Jain, S. K. [2 ]
Dobhal, D. P. [1 ]
Kumar, Amit [3 ]
机构
[1] Wadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
[2] Natl Inst Hydrol, Roorkee 247667, Uttar Pradesh, India
[3] Indian Agr Res Inst, Ctr Environm Sci & Climate Resilience Agr, New Delhi 110012, India
关键词
Beas River; hydrograph; snow/glacier melts runoff; SNOWMOD; LARGE HIMALAYAN BASIN; WESTERN HIMALAYA; CLIMATE-CHANGE; GLACIER-MELT; VARIABILITY; RUNOFF;
D O I
10.2166/wcc.2015.107
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In the present study, an attempt has been made to estimate the snow/glacier melt contribution in the head water region of the Beas Basin using a conventional hydrograph approach and a modeling (SNOWMOD) technique. The discharge and other meteorological data from 1996 to 2008 of the Manali site were used for the study. The results of SNOWMOD modeling reveal that snow/glacier melt contribution to the Beas River in the head water region varied between 52 (minimum) and 56% (maximum) with an annual average of 54% during the study period. The results obtained using the conventional approach showed the contribution of snow/glacier melt varied between 48 (minimum) and 52% (maximum) with an annual average of 50%. Results obtained using both techniques corroborate each other. This study reveals that the Beas River is mainly sustained by the snow/glacier melt contribution in the head water region.
引用
收藏
页码:880 / 890
页数:11
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