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DOI10.3390/rs13030497
Current Status and Variation since 1964 of the Glaciers around the Ebi Lake Basin in the Warming Climate
Wang, Lin; Bai, Changbin; Ming, Jing
通讯作者Ming, J (通讯作者),Beacon Sci & Consulting, Malvern, SA 5061, Australia.
发表日期2021
EISSN2072-4292
卷号13期号:3
英文摘要This work analyzed the spatial and temporal variations of the glaciers in the Ebi Lake basin during the period 1964 to 2019, based on the 1st and 2nd Chinese Glacier Inventories (CGI) and remote sensing data; this is believed to be the first long-term comprehensive remote sensing investigation on the glacier change in this area, and it also diagnosed the response of the glaciers to the warming climate by analyzing digital elevation modeling and meteorology. The results show that there are 988 glaciers in total in the basin, with a total area of 560 km(2) and average area of 0.57 km(2) for a single glacier. The area and number of the glaciers oriented north and northeast are 205 km(2) (327 glaciers) and 180 km(2) (265 glaciers), respectively. The glaciers are categorized into eight classes as per their area, which are less than 0.1, 0.1-0.5, 0.5-1.0, 1.0-2.0, 2.0-5.0, 5.0-10.0, 10.0-20.0, and greater than 20.0 km(2), respectively. The smaller glaciers between 0.1 km(2) and 10.0 km(2) account for 509 km(2) or 91% in total area, and, in particular, the glaciers smaller than 0.5 km(2) account for 74% in the total number. The glacial area is concentrated at 3500-4000 m in altitude (512 km(2) or 91.4% in total). The number of glaciers in the basin decreased by 10.5% or 116, and their area decreased by 263.29 km(2) (-4.79 km(2) a(-1)) or 32% (-0.58% a(-1)) from 1964 to 2019; the glaciers with an area between 2.0 km(2) and 5.0 km(2) decreased by the largest, -82.60 km(2) or -40.67% in the total area at -1.50 km(2) a(-1) or -0.74% a(-1)), and the largest decrease in number (i.e., 126 glaciers) occurs between 0.1 km(2) and 0.5 km(2). The total ice storage in the basin decreased by 97.84-153.22 km(3) from 1964 to 2019, equivalent to 88.06-137.90 km(3) water (taking 0.9 g cm(-3) as ice mass density). The temperature increase rate in the basin was +0.37 degrees C decade(-1), while the precipitation was +13.61 mm decade(-1) during the last fifty-five years. This analysis shows that the increase in precipitation in the basin was not sufficient to compensate the mass loss of glaciers caused by the warming during the same period. The increase in temperature was the dominant factor exceeding precipitation mass supply for ruling the retreat of the glaciers in the entire basin.
关键词TIEN-SHANMOUNTAINSDATABASERISE
英文关键词Ebi Lake basin; decelerated-melting glaciers; climate change; climate response
语种英语
WOS研究方向Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Remote Sensing ; Imaging Science & Photographic Technology
WOS记录号WOS:000615519600001
来源期刊REMOTE SENSING
来源机构中国科学院西北生态环境资源研究院
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/254518
作者单位[Wang, Lin; Bai, Changbin] Chinese Acad Sci, State Key Lab Cryospher Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China; [Ming, Jing] Beacon Sci & Consulting, Malvern, SA 5061, Australia
推荐引用方式
GB/T 7714
Wang, Lin,Bai, Changbin,Ming, Jing. Current Status and Variation since 1964 of the Glaciers around the Ebi Lake Basin in the Warming Climate[J]. 中国科学院西北生态环境资源研究院,2021,13(3).
APA Wang, Lin,Bai, Changbin,&Ming, Jing.(2021).Current Status and Variation since 1964 of the Glaciers around the Ebi Lake Basin in the Warming Climate.REMOTE SENSING,13(3).
MLA Wang, Lin,et al."Current Status and Variation since 1964 of the Glaciers around the Ebi Lake Basin in the Warming Climate".REMOTE SENSING 13.3(2021).
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