Recent regional warming across the Siberian lowlands: a comparison between permafrost and non-permafrost areas
文献类型:期刊论文
作者 | Wang,Ping3,4; Huang,Qiwei3,4; Liu,Shiqi4; Cai,Hongyan3,4; Yu,Jingjie3,4; Wang,Tianye2; Chen,Xiaolong1,6; Pozdniakov,Sergey P5 |
刊名 | Environmental Research Letters
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出版日期 | 2022-05-01 |
卷号 | 17期号:5 |
关键词 | climate warming permafrost degradation Siberian lowlands |
DOI | 10.1088/1748-9326/ac6c9d |
通讯作者 | Wang,Ping() ; Liu,Shiqi() |
英文摘要 | Abstract The northern mid-high latitudes experience climate warming much faster than the global average. However, the difference in the temperature change rates between permafrost and non-permafrost zones remains unclear. In this study, we investigated the temporal changes in temperature means and extremes across the Siberian lowlands (<500 m) over the past six decades (1960–2019) using in situ observations and reanalysis data. The results show that permafrost zones (0.39 °C/decade) have warmed faster than non-permafrost zones (0.31 °C/decade). The minimum values of the daily maximum (TXn) and minimum (TNn) temperatures changed faster than their maximum values (TXx, TNx), suggesting that low minimum temperatures increase faster, as evidenced by the considerably higher warming rate in the cool season (October–April, 0.43 ± 0.10 °C/decade, n= 126) than that in the warm season (May–September, 0.25 ± 0.08 °C/decade, n= 119). The change rates of TXx and TNx in permafrost areas were 2–3 times greater than those in non-permafrost areas; however, over the last ten years, TXx and TNx in non-permafrost areas showed decreasing trends. Moreover, faster-warming permafrost regions do not exhibit a faster increase in surface net solar radiation than slower-warming non-permafrost regions. While our findings suggest that carbon emissions from thawing soils are likely a potential driver of rapid warming in permafrost-dominated regions, the potential feedback between ground thawing and climate warming in permafrost regions remains uncertain. |
语种 | 英语 |
WOS记录号 | IOP:ERL_17_5_054047 |
出版者 | IOP Publishing |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/166818] ![]() |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Wang,Ping; Liu,Shiqi |
作者单位 | 1.CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, People’s Republic of China 2.School of Water Conservancy Engineering, Zhengzhou University, 100 Science Avenue, Zhengzhou, Henan 450001, People’s Republic of China 3.University of Chinese Academy of Sciences, Beijing 100049, People’s Republic of China 4.Key Laboratory of Water Cycle and Related Land Surface Processes, State Key Laboratory of Resources and Environmental Information Systems, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, 11A, Datun Road, Chaoyang District, Beijing 100101, People’s Republic of China 5.Department of Hydrogeology, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow 119899, Russia 6.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, People’s Republic of China |
推荐引用方式 GB/T 7714 | Wang,Ping,Huang,Qiwei,Liu,Shiqi,et al. Recent regional warming across the Siberian lowlands: a comparison between permafrost and non-permafrost areas[J]. Environmental Research Letters,2022,17(5). |
APA | Wang,Ping.,Huang,Qiwei.,Liu,Shiqi.,Cai,Hongyan.,Yu,Jingjie.,...&Pozdniakov,Sergey P.(2022).Recent regional warming across the Siberian lowlands: a comparison between permafrost and non-permafrost areas.Environmental Research Letters,17(5). |
MLA | Wang,Ping,et al."Recent regional warming across the Siberian lowlands: a comparison between permafrost and non-permafrost areas".Environmental Research Letters 17.5(2022). |
入库方式: OAI收割
来源:地理科学与资源研究所
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