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首页> 外文期刊>Journal of water and climate change >Estimation of snow/glacier melt contribution in the upper part of the Beas River basin, Himachal Pradesh, using conventional and SNOWMOD modeling approach
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Estimation of snow/glacier melt contribution in the upper part of the Beas River basin, Himachal Pradesh, using conventional and SNOWMOD modeling approach

机译:使用常规和SNOWMOD建模方法估算喜马al尔邦比斯河流域上部的雪/冰川融化贡献

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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.
机译:在本研究中,已经尝试使用常规的水文法和模型(SNOWMOD)技术来估算比斯盆地上游水域的雪/冰川融化贡献。该研究使用了Manali站点1996年至2008年的流量和其他气象数据。 SNOWMOD模型的结果表明,在研究期间,对上游水域的比斯河的冰雪融化贡献在52(最小)和56%(最大)之间变化,年平均为54%。使用常规方法获得的结果表明,雪/冰川融化的贡献在48(最小)和52%(最大)之间变化,年平均为50%。使用这两种技术获得的结果相互证实。这项研究表明,比斯河主要受上游水域冰雪融化的影响。

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