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	Glacier shrinkage in the Daxue and Danghenan ranges of the western Qilian Mountains, China, from 1957 to 2010
	Wang, Puyu1,2; Li, Zhongqin1,2,3; Yu, Guobin4; Li, Huilin1,2; Wang, Wenbin1; Huai, Baojuan1; Zhou, Ping1; Jin, Shuang1; Wang, Lin1; Zhang, Hui1
刊名	ENVIRONMENTAL EARTH SCIENCES
	2016
卷号	75期号:2页码:11
关键词	Fractal analysis Glacier change Regional differences Western Qilian Mountains
ISSN号	1866-6280
DOI	10.1007/s12665-015-5088-x
通讯作者	Wang, Puyu(wangpuyu@lzb.ac.cn)
英文摘要	Changes in glaciers in the Daxue and Danghenan ranges were analyzed based on topographic maps, satellite images and a digital elevation model (DEM). The results indicate that from 1957/ 1966 to 2010, the total area and ice volume for the investigated glaciers declined by 17.21 and 24.10 % in these respective ranges. From 1957 to 2010, the total area and ice volume in the glaciers in the Daxue Range declined by 16.03 % (0.30 % a(-1)) and 22.40 %, respectively, with a mean reduction of 0.133 km(2) for an individual glacier. These glaciers retreated by an average of 258 m (3.4 m a(-1)). From 1966 to 2010, the total area and ice volume for the glaciers in the Danghenan Range declined by 18.32 % (0.42 % a(-1)) and 25.70 %, with a mean reduction of 0.111 km(2) for an individual glacier. These glaciers retreated by an average of 159 m (3.6 m a(-1)). The rate of glacier retreat on the south-facing slopes was faster than that on the north-facing slopes. The area of glaciers on the south and north slopes of the Daxue Range declined by 22.82 and 15.51 %, respectively, and the area of glaciers on the south and north slopes of the Danghenan Range declined by 22.39 and 16.76 %, respectively. An analysis of the general trend of climatic change in the study area revealed that rapidly rising air temperatures were most likely the major factor causing the loss of glacier ice within the study area. Compared with other glaciers in the eastern and middle Qilian Mountains, glaciers in the western Qilian Mountains appeared to be losing mass at a slower rate. The differences of glacier changes in the eastern, middle, and western Qilian Mountains are mainly caused by the combination of climatic conditions and glacier morphologic factors.
收录类别	SCI
WOS关键词	RUNOFF ; LAKE
WOS研究方向	Environmental Sciences & Ecology ; Geology ; Water Resources
WOS类目	Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
语种	英语
出版者	SPRINGER
WOS记录号	WOS:000370240800038
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2557416
专题	寒区旱区环境与工程研究所
通讯作者	Wang, Puyu
作者单位	1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Tianshan Glaciol Stn, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China 2.Rhein Westfal TH Aachen, D-52056 Aachen, Germany 3.Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Peoples R China 4.Gansu Fundamental Geog Informat Ctr, Lanzhou 730000, Peoples R China
推荐引用方式 GB/T 7714	Wang, Puyu,Li, Zhongqin,Yu, Guobin,et al. Glacier shrinkage in the Daxue and Danghenan ranges of the western Qilian Mountains, China, from 1957 to 2010[J]. ENVIRONMENTAL EARTH SCIENCES,2016,75(2):11.
APA	Wang, Puyu.,Li, Zhongqin.,Yu, Guobin.,Li, Huilin.,Wang, Wenbin.,...&Zhang, Hui.(2016).Glacier shrinkage in the Daxue and Danghenan ranges of the western Qilian Mountains, China, from 1957 to 2010.ENVIRONMENTAL EARTH SCIENCES,75(2),11.
MLA	Wang, Puyu,et al."Glacier shrinkage in the Daxue and Danghenan ranges of the western Qilian Mountains, China, from 1957 to 2010".ENVIRONMENTAL EARTH SCIENCES 75.2(2016):11.

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