中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Permafrost degradation and its environmental effects on the Tibetan Plateau: A review of recent research

文献类型:期刊论文

作者Yang, Meixue1,2; Nelson, Frederick E.2; Shiklomanov, Nikolay I.3; Guo, Donglin4; Wan, Guoning1
刊名EARTH-SCIENCE REVIEWS
出版日期2010-11-01
卷号103期号:1-2页码:31-44
ISSN号0012-8252
关键词Active layer China Tibetan Plateau Permafrost Climate warming Permafrost degradation
DOI10.1016/j.earscirev.2010.07.002
通讯作者Yang, Meixue(mxyang@lzb.ac.cn)
英文摘要A significant portion of the Tibetan Plateau is underlain by permafrost, and is highly sensitive to climate change. Observational data from recent Chinese investigations on permafrost degradation and its environmental effects in the Tibetan region indicate that a large portion of the Tibetan Plateau has experienced significant warming since the mid-1950s. The air temperature increase is most significant in the central, eastern, and northwestern parts of the Plateau. The warming trend in the cold season was greater than that in the warm season. The duration of seasonal ground freezing has shortened due to the air temperature increase in winter. Numerical simulations indicate that air temperature on the Plateau will continue to increase in the 21st century. Significant warming has resulted in extensive degradation of permafrost Over the last 30 years, a 25 m increase in the lower altitudinal occurrences of permafrost has taken place in the north. In the south the increase is 50-80 m over the past 20 years. Active-layer thickness and mean annual ground temperature have increased by 0.15-0.50 m during 1996-2001 and by 0.1-0.5 degrees C during the last 30 years on the Tibetan Plateau, respectively. Widespread permafrost degradation has already caused environmental deterioration. Extensive desertification processes are apparent in the eastern and western portions of the Tibetan Plateau, with the area occupied by desert increasing annually by about 1.8%. With rapid retreat and thinning of permafrost, large carbon pools sequestered in permafrost could be released to increase net sources of atmospheric carbon, creating a positive feedback and accelerated warming. Damage to human infrastructure is also caused by frost heave, thaw settlement, and thaw slumping in the permafrost-affected region. The impact of permafrost degradation on energy and water exchange processes between the ground and atmosphere require further examination. Large-scale intensive monitoring networks, remote sensing investigations, and models for frozen soil are needed to clarify regional details of climate change, permafrost degradation, and their environmental effects. (c) 2010 Elsevier B.V. All rights reserved.
收录类别SCI
WOS关键词GROUND-PENETRATING RADAR ; HIGH-ALTITUDE PERMAFROST ; ASIAN SUMMER MONSOON ; EURASIAN SNOW COVER ; CLIMATE-CHANGE ; TEMPERATURE-CHANGE ; AIR-TEMPERATURE ; GREENHOUSE-GAS ; CHINA ; HIGHWAY
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000285074700002
URI标识http://www.irgrid.ac.cn/handle/1471x/2556440
专题寒区旱区环境与工程研究所
通讯作者Yang, Meixue
作者单位1.Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
2.Univ Delaware, Dept Geog, Newark, DE 19716 USA
3.George Washington Univ, Dept Geog, Washington, DC 20052 USA
4.Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Yang, Meixue,Nelson, Frederick E.,Shiklomanov, Nikolay I.,et al. Permafrost degradation and its environmental effects on the Tibetan Plateau: A review of recent research[J]. EARTH-SCIENCE REVIEWS,2010,103(1-2):31-44.
APA Yang, Meixue,Nelson, Frederick E.,Shiklomanov, Nikolay I.,Guo, Donglin,&Wan, Guoning.(2010).Permafrost degradation and its environmental effects on the Tibetan Plateau: A review of recent research.EARTH-SCIENCE REVIEWS,103(1-2),31-44.
MLA Yang, Meixue,et al."Permafrost degradation and its environmental effects on the Tibetan Plateau: A review of recent research".EARTH-SCIENCE REVIEWS 103.1-2(2010):31-44.

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来源:寒区旱区环境与工程研究所

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