Accelerating permafrost collapse on the eastern Tibetan Plateau

被引:34
|
作者
Gao, Tanguang [1 ]
Zhang, Yulan [2 ,3 ]
Kang, Shichang [2 ,3 ]
Abbott, Benjamin W. [4 ]
Wang, Xiaoming [2 ]
Zhang, Tingjun [1 ]
Yi, Shuhua [2 ,5 ]
Gustafsson, Orjan [6 ,7 ]
机构
[1] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China
[2] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China
[3] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[4] Brigham Young Univ, Dept Plant & Wildlife Sci, Provo, UT 84602 USA
[5] Nantong Univ, Sch Geog Sci, Inst Fragile Ecosyst & Environm, Nantong 226019, Peoples R China
[6] Stockholm Univ, Dept Environm Sci, S-10691 Stockholm, Sweden
[7] Stockholm Univ, Bolin Ctr Climate Res, S-10691 Stockholm, Sweden
基金
欧洲研究理事会; 中国国家自然科学基金;
关键词
permafrost; climate change; soil organic carbon; Tibetan Plateau;
D O I
10.1088/1748-9326/abf7f0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Permafrost collapse can rapidly change regional soil-thermal and hydrological conditions, potentially stimulating production of climate-warming gases. Here, we report on rate and extent of permafrost collapse on the extensive Tibetan Plateau, also known as the Asian Water Tower and the Third Pole. Combined data from in situ measurements, unmanned aerial vehicles (UAV), manned aerial photographs, and satellite images suggest that permafrost collapse was accelerating across the Eastern Tibetan Plateau. From 1969 to 2017, the area of collapsed permafrost has increased by approximately a factor of 40, with 70% of the collapsed area forming since 2004. These widespread perturbations to the Tibetan Plateau permafrost could trigger changes in local ecosystem state and amplify large-scale permafrost climate feedbacks.
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收藏
页数:11
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