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
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机构:
Wadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, IndiaWadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
Ahluwalia, Rajeev Saran
[1
]
Rai, S. P.
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机构:
Natl Inst Hydrol, Roorkee 247667, Uttar Pradesh, IndiaWadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
Rai, S. P.
[2
]
Jain, S. K.
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机构:
Natl Inst Hydrol, Roorkee 247667, Uttar Pradesh, IndiaWadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
Jain, S. K.
[2
]
Dobhal, D. P.
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Wadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, IndiaWadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
Dobhal, D. P.
[1
]
Kumar, Amit
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机构:
Indian Agr Res Inst, Ctr Environm Sci & Climate Resilience Agr, New Delhi 110012, IndiaWadia Inst Himalayan Geol, Ctr Glaciol, Dehra Dun 248001, Uttar Pradesh, India
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
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.