Glacier variations in response to climate change from 1972 to 2007 in the western Lenglongling mountains, northeastern Tibetan Plateau

被引:26
|
作者
Pan, Baotian [1 ]
Cao, Bo [1 ]
Wang, Jie [1 ]
Zhang, Guoliang [1 ]
Zhang, Chen [1 ]
Hu, Zhenbo [1 ]
Huang, Bo [1 ]
机构
[1] Lanzhou Univ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
基金
中国国家自然科学基金; 美国国家科学基金会;
关键词
SEA-LEVEL RISE; SATELLITE IMAGERY; AERIAL PHOTOGRAPHS; PATAGONIA ICEFIELD; SOUTHERN PATAGONIA; CORDILLERA BLANCA; ELEVATION CHANGES; NORTHWEST CHINA; ICE-ELEVATION; QILIAN SHAN;
D O I
10.3189/2012JoG12J032
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Global warming is causing widespread glacier retreat, with small glaciers disappearing. We investigate changes in glaciers over the western Lenglongling mountains, located in the northeastern margin of the Tibetan Plateau. Glacier extent over the western Lenglongling mountains is estimated by comparing digitized glacier outlines obtained from aerial photographs and satellite imagery. These results suggest that all 179 glaciers in the western Lenglongling mountains shrunk between 1972 and 2007. The total area loss was similar to 24.4 km(2), accounting for similar to 28.3% (0.81% a(-1)) of the glacierized area in 1972. The average area retreat rates differ over different time intervals: they are approximately 0.68, 0.90, 0.77 and 0.56 km(2) a(-1) over the periods 1972-95, 1995-99, 1999-2002 and 2002-07, respectively. Based on analysis of meteorological data, glacier shrinkage in the study area can probably be attributed to the increase in air temperature. Furthermore, the smaller glaciers display a higher shrinkage rate than larger glaciers, and glaciers on southwest-facing slopes appear to retreat faster than those on northeast-facing slopes.
引用
收藏
页码:879 / 888
页数:10
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