[1]牛竞飞,刘景时,王迪,等.2009年喀喇昆仑山叶尔羌河冰川阻塞湖及冰川跃动监测[J].山地学报,2011,(03):276.
NIU Jingfei,LIU Jingshi,et al.Monitoring on Icedammed Lake and Related Surging Glaciers in Yarkant River, Karakorum in 2009[J].Mountain Research,2011,(03):276.
点击复制
2009年喀喇昆仑山叶尔羌河冰川阻塞湖及冰川跃动监测()
《山地学报》[ISSN:1008-2186/CN:51-1516]
- 卷:
-
- 期数:
-
2011年03期
- 页码:
-
276
- 栏目:
-
山地学报
- 出版日期:
-
2011-01-01
文章信息/Info
- Title:
-
Monitoring on Icedammed Lake and Related Surging Glaciers in Yarkant River, Karakorum in 2009
- 作者:
-
牛竞飞;刘景时;王迪;Kenneth Hewitt;
-
1.中国科学院青藏高原研究所,北京 100085;
2.中国科学院研究生院,北京 100049;
3. Cold Regions Research Centre, Wilfrid Laurier University, Waterloo, Ontario N2L3C5, Canada
- Author(s):
-
NIU Jingfei; LIU Jingshi; WANG Di; Kenneth Hewitt
-
1. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing100085, China;
2. Graduate University, Chinese Academy of Sciences, Beijing100049, China;
3. Cold Regions Research Centre, Wilfrid Laurier University, Waterloo, Ontario N2L3C5, Canada
-
- 关键词:
-
喀喇昆仑山; 冰川阻塞湖; 冰川跃动; 环境一号; SPOT
- Keywords:
-
Karakorum; icedammed lake; glacier surging; HJ-1A/1B; SPOT
- 分类号:
-
P931.4
- 文献标志码:
-
A
- 摘要:
-
在气候变化的影响下,喀喇昆仑山叶尔羌河冰川突发洪水近几年频繁发生。2009-05—09,利用中国环境减灾卫星(HJ-1A/1B)影像,对叶尔羌河上游冰川突发洪水的源头进行了动态监测。在克亚吉尔冰川末端发现了冰川阻塞湖,并监测到其不断扩大。2009-08初该处冰川湖突然消失,同期影像显示其消失后,河谷中残留大量冰体,与往年情况差异巨大。结合相关水文记录及历史资料分析认为,极有可能是冰川末端突然前进(跃动)使冰川坝遭到破坏,导致冰川阻塞湖泄水。由此推测克亚吉尔冰川发生了罕见跃动现象,但需要进一步研究验证。
- Abstract:
-
Under the influence of climate and glacier changes, Glacier Lake Outburst Floods (GLOFs) occurred frequently in Yarkant River, Karakorum,China, in recent years. Using China Environment and Natural Disaster Monitoring Satellite images (HJ-1A/1B), source of floods in upstream Yarkant River was under dynamic monitoring from May to September in 2009. During this period, an expanding icedammed lake was found in the glacier terminus of Kyagar. However, in early August the icedammed lake suddenly disappeared, leaving a large number of ices in the river valley. This phenomenon is significant different from previous years. Related hydrological records and analysis of historical data show a sudden advancing of glacier terminus damaged the ice dam, leading to the leak out of icedammed lake. The results suggested that infrequent glacier surging occurred in Kyagar glacier, and further monitoring will be conducted near future.
备注/Memo
- 备注/Memo:
-
收稿日期(Received date):2010-11-21;改回日期(Accepted) : 2011-04-02。
基金项目(Foundation item):国家重点基础研究发展计划(973计划)项目(2007CB411503);国家自然科学基金(40971047);中国科学院知识创新工程重要方向项目(KZCX2-YW-310);科技部攻关项目(2006FY110200)资助。\[Supposed by National Program on Key Basic Research Project (973 Program) (2007CB411503), National Natural Science Foundation of China (40971047), Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-310) and National Key Technologies R & D Program of China (2006FY110200).\]
作者简介(Biography):牛竞飞(1986-),男,山东东营人,硕士研究生,主要从事冰川水文水资源研究。\[Niu Jingfei(1986-), Male, Master degree candidate, mainly engaged in glacier hydrology and water resources.\] E-mail: niujingfei@itpcas.ac.cn
更新日期/Last Update:
1900-01-01