Comparison of changes in glacier area and thickness on the northern and southern slopes of Mt. Bogda, eastern Tianshan Mountains

被引:11
作者
Wang, Puyu [1 ,2 ]
Li, Zhongqin [1 ,2 ,3 ]
Wang, Wenbin [1 ]
Li, Huilin [1 ,2 ]
Wu, Lihua [4 ]
Huai, Baojuan [1 ]
Zhou, Ping [1 ]
Jin, Shuang [1 ]
Wang, Lin [1 ]
机构
[1] Chinese Acad Sci, State Key Lab Cryosphere Sci, Cold & Arid Reg Environm & Engn Res Inst, Tianshan Glaciol Stn, 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] Southwest Forestry Univ, Fac Ecotourism, Kunming 6500224, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Ice thickness; Glacier volume; Glacier variation; Climate change; Mt; Bogda; Eastern Tianshan Mountains; TIEN-SHAN; CLIMATE-CHANGE; MASS-BALANCE; CENTRAL-ASIA; VOLUME; SENSITIVITY; PATAGONIA; RETREAT; CANADA; CHINA;
D O I
10.1016/j.jappgeo.2016.07.009
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Rapid shrinkage and dramatic volume loss of the glaciers on Mt. Bogda in the eastern Tianshan Mountains have resulted in water shortages in the surrounding arid regions of China. Understanding ice thickness and its variation is important to the analysis of changes in glacial volume, which are directly related to regional hydrology and water resources. Fan-shaped Diffluence Glacier and Heigou Glacier No. 8 are located on the northern and southern slopes of Mt. Bogda, respectively. In this paper, the spatial distribution of the ice thickness of these two glaciers and the changes in their area and volume are discussed based on a 2009 survey result and comparison to previous investigations. The mean ice thickness of the tongue of Fan-shaped Diffluence Glacier was about 823 m and the calculated ice volume was 385.2 x 10(6) m(3) in 2009. It had thinned by 14 +/- 8 m (0.30 +/- 0.17 m a(-1)) from 1962 to 2009, equivalent to an ice volume loss of 65.5 +/- 37.4 x 10(6) m(3). The mean ice thickness of the tongue of Heigou Glacier No. 8 was 58.7 m and the calculated ice volume was 115.1 x 10(6) m(3) in 2009. The tongue of Heigou Glacier No. 8 thinned by 13 6 m (0.57 +/- 0.26 m a(-1)) from 1986 to 2009, which corresponds to an ice volume loss of 25.5 +/- 11.8 x 10(6) m(3). The greater thinning and retreat of Heigou Glacier No. 8 than those of Fan-shaped Diffluence Glacier is partially due to topographic characteristics. The difference can be attributed mainly to the greater increase in temperature on the southern slope than on the northern slope. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:164 / 173
页数:10
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