西喜马拉雅地区气候驱动的变化:预计冰川撤退,雪地覆盖的变化以及未来的融化水流量

Japjeet Singh1, Vishal Singh2, Chandra Shekhar Prasad Ojha1

  • 1Department of Civil Engineering, Indian Institute of Technology Roorkee, Uttarakhand, India.

概括

喜马拉雅山的变暖加剧了冰川的融化,改变了河流的流动. 这项研究模拟了上甘流域,预计到2100年冰川融化减少,因降雨模式变化而增加洪水/干旱风险.

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