《Table 3 Regional contribution to air temperature changes in China during different periods》

  提示：宽带有限、当前游客访问压缩模式

本系列图表出处文件名：随高清版一同展现

《中国气温变化对全球变暖停滞的响应（英文）》

1. 获取 高清版本忘记账户？点击这里登录

1. 下载图表忘记账户？点击这里登录

Comparing the trends found nationally and for the three geographic zones in China（Figure 8），we find significant differences in the responses of the three geographic zones to the global warming hiatus.Generally，the three geographic zones showed significant warming trends for 1960–2016，1960–1998，and 1960–2012.The eastern monsoon and northwestern arid regions showed significant cooling trends over 1998–2012，and the cooling rates exceeded the national average.The northwestern arid region contributed the most，46.98%and–0.361℃/10a，followed by the eastern monsoon region，53.79%and–0.31℃/10a（Table 3）；clearly，both areas responded significantly to the hiatus.However，in the Tibetan Plateau，the warming rate was 0.204℃/10a for 1998–2012，which was slightly higher than 1960–1998，slightly lower than 1960–2012；the temperature fluctuations were not significant in other time periods，but the warming was much higher than the warming rate in the eastern monsoon and northwest arid regions during the same period.The Tibetan Plateau contributed–70%without the warming hiatus（Table 3）.Duan et al.（2016）pointed out that the temperature and precipitation on the Tibetan Plateau accelerated under the background of global warming.The results from this study show that the high frigid region of the Tibetan Plateau warmed at a higher rate in different periods.Before 1998，the contribution to warming temperatures was smaller than that from the eastern monsoon and northwest arid regions，but far exceeded the national average after 1998.Particularly after 2000，the warming rate reached a new peak.