中国气温变化对全球变暖停滞的响应(英文)
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  • 英文篇名:Changes in air temperature over China in response to the recent global warming hiatus
  • 作者:杜勤勤 ; 张明军 ; 王圣杰 ; 车存伟 ; 马荣 ; 马转转
  • 英文作者:DU Qinqin;ZHANG Mingjun;WANG Shengjie;CHE Cunwei;MA Rong;MA Zhuanzhuan;College of Geography and Environmental Science, Northwest Normal University;
  • 英文关键词:global warming hiatus;;three geographic zones;;temperature;;China
  • 中文刊名:ZGDE
  • 英文刊名:地理学报(英文版)
  • 机构:College of Geography and Environmental Science,Northwest Normal University;
  • 出版日期:2019-03-14
  • 出版单位:Journal of Geographical Sciences
  • 年:2019
  • 期:v.29
  • 基金:National Basic Research Program of China(973 Program),No.2013CBA01801;; Promotion Project for Young Teachers in Northwest Normal University,No.NWNU-LKQN-15-8
  • 语种:英文;
  • 页:ZGDE201904002
  • 页数:21
  • CN:04
  • ISSN:11-4546/P
  • 分类号:18-38
摘要
The 1998–2012 global warming hiatus has aroused great public interest over the past several years. Based on the air temperature measurements from 622 meteorological stations in China, the temperature response to the global warming hiatus was analyzed at national and regional scales. We found that air temperature changed –0.221℃/10 a during 1998–2012, which was lower than the long-term trend for 1960–1998 by 0.427℃/10 a. Therefore, the warming hiatus in China was more pronounced than the global mean. Winter played a dominant role in the nationwide warming hiatus, contributing 74.13%, while summer contributed the least among the four seasons. Furthermore, the warming hiatus was spatial heterogeneous across different climate conditions in China. Comparing the three geographic zones, the monsoon region of eastern China, arid region of northwestern China, and high frigid region of the Tibetan Plateau, there was significant cooling in eastern and northwestern China. In eastern China, which contributed 53.79%, the trend magnitudes were 0.896℃/10 a in winter and 0.134℃/10 a in summer. In the Tibetan Plateau, air temperature increased by 0.204℃/10 a, indicating a lack of a significant warming hiatus. More broadly, the warming hiatus in China may have been associated with the negative phase of PDO and reduction in sunspot numbers and total solar radiation. Finally, although a warming hiatus occurred in China from 1998 to 2012, air temperature rapidly increased after 2012 and will likely to continuously warm in the next few years.
        The 1998–2012 global warming hiatus has aroused great public interest over the past several years. Based on the air temperature measurements from 622 meteorological stations in China, the temperature response to the global warming hiatus was analyzed at national and regional scales. We found that air temperature changed –0.221℃/10 a during 1998–2012, which was lower than the long-term trend for 1960–1998 by 0.427℃/10 a. Therefore, the warming hiatus in China was more pronounced than the global mean. Winter played a dominant role in the nationwide warming hiatus, contributing 74.13%, while summer contributed the least among the four seasons. Furthermore, the warming hiatus was spatial heterogeneous across different climate conditions in China. Comparing the three geographic zones, the monsoon region of eastern China, arid region of northwestern China, and high frigid region of the Tibetan Plateau, there was significant cooling in eastern and northwestern China. In eastern China, which contributed 53.79%, the trend magnitudes were 0.896℃/10 a in winter and 0.134℃/10 a in summer. In the Tibetan Plateau, air temperature increased by 0.204℃/10 a, indicating a lack of a significant warming hiatus. More broadly, the warming hiatus in China may have been associated with the negative phase of PDO and reduction in sunspot numbers and total solar radiation. Finally, although a warming hiatus occurred in China from 1998 to 2012, air temperature rapidly increased after 2012 and will likely to continuously warm in the next few years.
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