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DOI10.5194/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
ISSN1994-0416
EISSN1994-0424
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).
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