Climate Change Data Portal
DOI | 10.5194/tc-15-199-2021 |
Response of downstream lakes to Aru glacier collapses on the western Tibetan Plateau | |
Lei, Yanbin; Yao, Tandong; Tian, Lide; Sheng, Yongwei; Liao, Jingjuan; Zhao, Huabiao; Yang, Wei; Yang, Kun; Berthier, Etienne; Brun, Fanny; Gao, Yang; Zhu, Meilin; Wu, Guangjian | |
通讯作者 | Lei, YB (通讯作者) |
发表日期 | 2021 |
ISSN | 1994-0416 |
EISSN | 1994-0424 |
起始页码 | 199 |
结束页码 | 214 |
卷号 | 15期号:1 |
英文摘要 | The lower parts of two glaciers in the Am range on the western Tibetan Plateau (TP) collapsed on 17 July and 21 September 2016, respectively, causing fatal damage to local people and their livestock. The giant ice avalanches, with a total volume of 150 x 10(6) m(3), had almost melted by September 2019 (about 30 % of the second ice avalanche remained). The impact of these extreme disasters on downstream lakes has not been investigated yet. Based on in situ observation, bathymetry survey and satellite data, we explore the impact of the ice avalanches on the two downstream lakes (i.e., Am Co and Memar Co) in terms of lake morphology, water level and water temperature in the subsequent 4 years (2016-2019). After the first glacier collapse, the ice avalanche slid into Aru Co along with a large amount of debris, which generated great impact waves in Aru Co and significantly modified the lake's shoreline and underwater topography. An ice volume of at least 7.1 x 10(6) m(3 )was discharged into Aru Co, spread over the lake surface and considerably lowered its surface temperature by 2-4 degrees C in the first 2 weeks after the first glacier collapse. Due to the large amount of meltwater input, Memar Co exhibited more rapid expansion after the glacier collapses (2016-2019) than before (2003-2014), in particular during the warm season. The melting of ice avalanches was found to contribute to about 23 % of the increase in lake storage between 2016 and 2019. Our results indicate that the Am glacier collapses had both short-term and long-term impacts on the downstream lakes and provide a baseline in understanding the future lake response to glacier melting on the TP under a warming climate. |
关键词 | DIGITAL ELEVATION MODELSHIGH-MOUNTAIN ASIAMASS BALANCESWATER-LEVELDYNAMICSOUTBURSTSTORAGECOKUNLUNREGION |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000611038600001 |
来源期刊 | CRYOSPHERE |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260536 |
推荐引用方式 GB/T 7714 | Lei, Yanbin,Yao, Tandong,Tian, Lide,et al. Response of downstream lakes to Aru glacier collapses on the western Tibetan Plateau[J]. 中国科学院青藏高原研究所,2021,15(1). |
APA | Lei, Yanbin.,Yao, Tandong.,Tian, Lide.,Sheng, Yongwei.,Liao, Jingjuan.,...&Wu, Guangjian.(2021).Response of downstream lakes to Aru glacier collapses on the western Tibetan Plateau.CRYOSPHERE,15(1). |
MLA | Lei, Yanbin,et al."Response of downstream lakes to Aru glacier collapses on the western Tibetan Plateau".CRYOSPHERE 15.1(2021). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。