How would global-mean temperature change in the 21st century?

查看全文 作　　者：QIAN [1]WeiHong;LU [1]Bo;ZHU [2]CongWen

机构地区：[1]Monsoon and Environment Research Group, School of Physics, Peking University, Beijing 100871, China;[2]Institute of Climate System, Chinese Academy of Meteorological Sciences, Beijing 100081, China

出　　处：《Chinese Science Bulletin》索引2010年第55卷第19期,共5页

基　　金：supported by the National Natural Science Foundation of China (90502001,90711003 and 40890053) 摘　　要：The time series of HadCRUT3 global-mean surface air temperature(GSAT) anomaly,Pacific decadal oscillation(PDO) index,and the equatorial Pacific sea surface temperature(SST) were utilized,and their long-term trends and multiple time-scale periodic oscillations were explored in this study.A long-term trend with a warming rate about 0.44°C /century during 1850-2008,two cool floors occurred respectively around 1910 and during 1950-1970,and three warm flats happened in the 1870s,1940s and since the year 1998 were found in the GSAT.In this duration,the variability of GSAT can be well reconstructed by the quasi-21-year,the quasi-65-year,and century-scale oscillations.The recent decadal warm flat is caused by their positive phase overlapping from these three oscillations.The maximum rising temperature reached 0.26°C was simulated in 2004 by the three oscillations.The quasi-21-year and the quasi-65-year oscillations were possibly caused by solar radiation and internal variability of the ocean-atmosphere system.Therefore,an outlook of GSAT for the 21st century was made based on the long-term trend and these three oscillations.It was expected that a cool floor and a warm flat of the GSAT would appear in the 2030s and 2060s,respectively.However,the highest warming range is predicted about 0.6°C,it is less than the threshold 2°C and IPCC projection. 关键词：平均温度太平洋年代际振荡大气系统气温上升赤道太平洋多时间尺度时间序列海表温度

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How would global-mean temperature change in the 21st century?

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