Response of "Glacier-Runoff" system in a typical monsoonal temperate glacier region, Hailuogou Basin in Mt. Gongga of China, to global warming

Zongxing Li (1) , Yuanqing He (1) , Xiaomei Yang (2) , Xianzhong He (1) , Hongxi Pang (1) , Wenxiong Jia (1) , Caixia Zhang (1) , Linlin Yuan (1) , Haoyu He (1) , Xinxin Zuo (1)

1 The State Key Laboratory of Cryosphere Science
2 College of Geography and Environment Science

The method of correlation analysis and trend analysis were used in this research in order to confirm the response of "glacier-runoff" system to global warming. Hailuogou glacier had retreated by 1871.8 m over the past 76 years, Hailuogou No. 2 glacier had also retreated by 1100 m. Glaciers retreats are contrary to the climatic warming trend in China and the Northern Hemisphere. Glaciers in Hailuogou basin were in the loss with a fluctuating manner since 1950s, and accumulative value of mass balance is ?10 825.5 mm water equivalent with an annual mean value of ?240.6 mm. The inverse correlation is highly significant between mass balance variation and climatic fluctuation of China and the Northern Hemisphere after 1950s. Glacier ablation is intensive with a ratio of 7.86 m yr^?1. A steady rise tendency toward glaciers runoff has been observed since 1980s, and the runoff rise is mainly responsible for melt water in Hailuogou basin. It is noticeable that climatic warming not only strengthened ablation extent and enlarged ablation area, but also prolonged ablation period. Global warming is the main cause of glacier retreat, mass loss and runoff rise in Hailuogou basin.

Domaines: Interfaces continentales, environnement; Océan, Atmosphère; Sciences de la Terre

Zongxing Li, Yuanqing He, Xiaomei Yang, Xianzhong He, Hongxi Pang, et al.. Response of "Glacier-Runoff" system in a typical monsoonal temperate glacier region, Hailuogou Basin in Mt. Gongga of China, to global warming. Hydrology and Earth System Sciences Discussions, 2007, 4 (5), pp.3395-3412. ⟨hal-00298894⟩