Projected glacier meltwater and river run‐off changes in the Upper Reach of the Shule River Basin, north‐eastern edge of the Tibetan Plateau

Glacier meltwater change in the north‐eastern edge of the Tibetan Plateau is greatly important for the projection of the impact of future climate change on local water resource management. Although the glaciated area is only approximately 4% of the Upper Reach of the Shule River Basin (URSRB), the a...

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Veröffentlicht in:Hydrological processes 2019-03, Vol.33 (7), p.1059-1074
Hauptverfasser: Zhang, Zhihua, Deng, Shifan, Zhao, Qiudong, Zhang, Shiqiang, Zhang, Xiaowen
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Sprache:eng
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