Glaciers in Xinjiang: Past Changes and Current Status
编号:1511 稿件编号:472 访问权限:仅限参会人 更新:2021-06-16 10:31:13 浏览:716次 特邀报告

报告开始:2021年07月11日 13:30 (Asia/Shanghai)

报告时间:20min

所在会议:[S16C] 16C、冰冻圈科学 » [S16C-1] 16C、冰冻圈科学-1

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摘要
The Xinjiang Uyghur Autonomous Region of China is the largest arid region in Central Asia, and is heavily dependent on glacier melt in high mountains for water supplies. In this paper, glacier and climate changes in Xinjiang during the past decades were comprehensively discussed based on glacier inventory data, individual monitored glacier observations, recent publications, as well as meteorological records. The results show that glaciers have been in continuous mass loss and dimensional shrinkage since the 1960s, although there are spatial differences between mountains and sub-regions, and the significant temperature increase is the dominant controlling factor of glacier change. The mass loss of monitored glaciers in the Tien Shan has accelerated since the late 1990s, but has a slight slowing after 2010. Remote sensing results also show a more negative mass balance in the 2000s and mass loss slowing in the latest decade (2010s) in most regions. This needs further investigation on whether the slowing is general and continuing. In addition, glacier surging occurs more frequently in the Karakoram and Kunlun Mountains.
 
关键字
glacier change; mass loss,climate change; Xinjiang; Central Asia
报告人
王璞玉
中国科学院西北生态环境资源研究院

稿件作者
王璞玉 中国科学院西北生态环境资源研究院
李宏亮 中国科学院西北生态环境资源研究院
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