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Authors
Affiliations
1 School of Resources and Environment Science, Xinjiang University, Urumqi 830046, CN
2 Jiang An Campus of Sichuan University, College of Architecture and Environment, Chengdu, 6102075, CN
3 Key Laboratory of Oasis Ecology, Ministry of Education, Xinjiang University, Urumqi 830046, CN
4 Xinjiang Institute of Ecology and Geography, Chinese Academy of Science, Urumqi 830011, CN
5 LREIS, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Science, Beijing 100101, CN
Source
Nature Environment and Pollution Technology, Vol 12, No 4 (2013), Pagination: 555-562
Abstract
A major proportion of discharge in the Juntanghu river basin is contributed by its glacier-fed river and snow catchments situated in northern mid-slope of Tianshan Mountain, Northwest China. The Mann-Kendall trend test based on the 50 years data (1961 to 2011) were used for analysis of the climate change trends and the application of the SWAT model under different climate change scenarios show that watershed hydrological cycle would alter under different climatic scenarios. This suggests that the reservoirs will be necessary for large flow storage to meet the need of the flood control, water supply, etc.
Keywords
Snowmelt Runoff, SWAT Analysis, Climate Change Effect, Tianshan Mountain.
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