中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatiotemporal Changes in Active Layer Thickness under Contemporary and Projected Climate in the Northern Hemisphere

文献类型:期刊论文

作者Peng, Xiaoqing1; Zhang, Tingjun1; Frauenfeld, Oliver W.2; Wang, Kang3; Luo, Dongliang4; Cao, Bin1; Su, Hang1; Jin, Huijun4; Wu, Qingbai4
刊名JOURNAL OF CLIMATE
出版日期2018
卷号31期号:1页码:251-266
ISSN号0894-8755
DOI10.1175/JCLI-D-16-0721.1
通讯作者Zhang, Tingjun(tjzhang@lzu.edu.cn)
英文摘要Variability of active layer thickness (ALT) in permafrost regions is critical for assessments of climate change, water resources, and engineering applications. Detailed knowledge of ALT variations is also important for studies on ecosystem, hydrological, and geomorphological processes in cold regions. The primary objective of this study is therefore to provide a comprehensive 1971-2000 climatology of ALT and its changes across the entire Northern Hemisphere from 1850 through 2100. To accomplish this, in situ observations, the Stefan solution based on a thawing index, and the edaphic factor (E factor) are employed to calculate ALT. The thawing index is derived from (i) the multimodel ensemble mean of 16 models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) over 1850-2005, (ii) three representative concentration pathways (RCP2.6, RCP4.5, and RCP8.5) for 2006-2100, and (iii) Climatic Research Unit (CRU) gridded observations for 1901-2014. The results show significant spatial variability in in situ ALT that generally ranges from 40 to 320 cm, with some extreme values of 900 cm in the Alps. The differences in the ALT climatology between the three RCPs and the historical experiments ranged from 0 to 200 cm. The biggest increases, of 120-200 cm, are on the Qinghai-Tibetan Plateau, while the smallest increases of less than 20 cm are in Alaska. Averaged over all permafrost regions, mean ALT from CMIP5 increased significantly at 0.57 +/- 0.04 cm decade(-1) during 1850-2005, while 2006-2100 projections show ALT increases of 0.77 +/- 0.08 cm decade(-1) for RCP2.6, 2.56 +/- 0.07 cm decade(-1) for RCP4.5, and 6.51 +/- 0.07 cm decade(-1) for RCP8.5.
收录类别SCI
WOS关键词SEASONAL SNOW COVER ; HEIHE RIVER-BASIN ; TIBETAN PLATEAU ; MACKENZIE VALLEY ; THERMAL REGIME ; WESTERN CHINA ; SEA-ICE ; PERMAFROST ; REGIONS ; CMIP5
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
出版者AMER METEOROLOGICAL SOC
WOS记录号WOS:000429528800014
URI标识http://www.irgrid.ac.cn/handle/1471x/2558145
专题寒区旱区环境与工程研究所
通讯作者Zhang, Tingjun
作者单位1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou, Gansu, Peoples R China
2.Texas A&M Univ, Dept Geog, College Stn, TX USA
3.Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA
4.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Peng, Xiaoqing,Zhang, Tingjun,Frauenfeld, Oliver W.,et al. Spatiotemporal Changes in Active Layer Thickness under Contemporary and Projected Climate in the Northern Hemisphere[J]. JOURNAL OF CLIMATE,2018,31(1):251-266.
APA Peng, Xiaoqing.,Zhang, Tingjun.,Frauenfeld, Oliver W..,Wang, Kang.,Luo, Dongliang.,...&Wu, Qingbai.(2018).Spatiotemporal Changes in Active Layer Thickness under Contemporary and Projected Climate in the Northern Hemisphere.JOURNAL OF CLIMATE,31(1),251-266.
MLA Peng, Xiaoqing,et al."Spatiotemporal Changes in Active Layer Thickness under Contemporary and Projected Climate in the Northern Hemisphere".JOURNAL OF CLIMATE 31.1(2018):251-266.

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来源:寒区旱区环境与工程研究所

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