Quantifying the contribution of climate and underlying surface changes to alpine runoff alterations associated with glacier melting |
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| Authors: | Jiali Xin Xiaoyu Sun Liu Liu Hao Li Xingcai Liu Xiuping Li Lei Cheng Zongxue Xu |
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| Institution: | 1. College of Water Resources and Civil Engineering, China Agricultural University, Beijing, China;2. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of China, Beijing, China;3. Institute of Tibetan Plateau Research, Chinese Academy of China, Beijing, China;4. State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, China;5. College of Water Sciences, Beijing Normal University, Beijing, China
Beijing Key Laboratory of Urban Hydrological Cycle and Sponge City Technology, Beijing, China |
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| Abstract: | Climate variability and underlying surface changes are strongly associated with runoff alterations. The Yarlung Zangbo River Basin (YZRB) is a typical alpine region located in the southeast Qinghai–Tibet Plateau, where runoff is particularly sensitive and vulnerable to climate and environmental changes. Here, we conducted a quantitative assessment of the contributions of climate variability and underlying surface changes to runoff alterations from 1966 to 2015 in the upper, middle, and lower regions of the YZRB. The year 1997 was identified as the runoff breakpoint in all three sub-regions, which divided the runoff time series into the baseline period (1966–1997) and change period (1998–2015). An adjusted Budyko framework accounting for glacier runoff was developed to conduct a runoff alteration attribution analysis. The results indicated that the increase in runoff in the upper region was dominated by changes in the underlying surface and glacier runoff, whose contribution accounted for 59.61 and 49.18%, respectively. The runoff increase in the middle and lower regions was mainly attributed to the increase in precipitation, accounting for 39.36 and 129.21% of the total runoff alteration, respectively. Moreover, due to the little variation in vegetation and degradation of permafrost in the upper region, increases in runoff might be largely attributed to increases in subsurface runoff caused by the melting of permafrost. In the middle region, in addition to increased precipitation, vegetation degradation had positive effects on runoff increases. The lower region exhibited far higher water consumption rates due to its extensive and dense vegetation coverage accompanied by rising temperature, which resulted in a negative contribution (−58.74%) to runoff alteration. Our findings may therefore have important implications for water resource security and sustainable development in alpine regions. |
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| Keywords: | Budyko climate change glacier permafrost Qinghai–Tibet Plateau runoff |
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