Major Controls on Streamflow of the Glacierized Urumqi River Basin in the Arid Region of Northwest China

Major Controls on Streamflow of the Glacierized Urumqi River Basin in the Arid Region of Northwest China
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西北干旱区乌鲁木齐河流域冰川化径流的主要控制

DOI:
10.3390/w12113062
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发表时间:
2020-11
期刊:
影响因子:
3.4
通讯作者:
Hong Fang
Hong Fang
中科院分区:
环境科学与生态学3区
文献类型:
--
作者:
Muattar Saydi;Guoping Tang;Hong Fang

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理解径流可利用性的主要驱动因素对水资源有限的内陆盆地具有重要意义,在这些地区,冰雪融化是地表径流的重要补给来源。本文对径流对……变化的响应进行了分析(原句中“in c”不完整,可能影响准确翻译)
Understanding the main drivers of runoff availability has important implications for water-limited inland basins, where snow and ice melt provide essential input to the surface runoff. This paper presents an analysis on the runoff response to changes in climatic and other controls of water-energy balance in an inland glacierized basin, the Urumqi River basin, located in the arid region of northwest China, and identifies the major control to which runoff is sensitive across the basin’s heterogeneous subzones. The results indicate that the runoff is more sensitive to change in precipitation in the mountainous headwaters zone of the upper reach, and followed by the impact of basin characteristics. In contrast, the runoff is more sensitive to changes in the basin characteristics in the semiarid and arid zones of the mid and lower reaches. In addition, the change in basin characteristics might be represented by the distinct glacier recession in the mountainous upper reach zone and the increasing human interferences, i.e., changes in land surface condition and population growth, across the mid and lower reach zones. The glacier wasting contributed around 7% on average to the annual runoff between 1960 and 2012, with an augmentation beginning in the mid-1990s. Findings of this study might help to better understand the possible triggers of streamflow fluctuation and the magnitude of glacier wasting contribution to runoff in inland glacierized river basins.
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