新疆水资源有80%以上形成于盆地周围的中高山区,其中高山地区的冰川和积雪融水是内陆河流的主要补给源,随着全球变化引起的高山寒区升温和降水变化在此反映敏感,已经显示出自20世纪80年代中期以来的异常变化.一方面,气温持续升高可以加速冰川消融,导致冰川面积缩小,冰厚减薄,运 Over 80% of Xinjiang’s water resources are formed in the middle and high mountain areas around the basin. Among them, glaciers and snowmelt melts in the mountainous areas are the main recharge sources of the inland rivers. As the global change causes the temperature and precipitation in alpine areas to change, Reflect sensitive, has shown the unusual changes since the mid-1980s, on the one hand, the continued temperature rise can accelerate the glacier ablation, resulting in reduced glacier area, thin ice thickness, transport