Evaluation of East Asian climatology as simulated by seven coupled models

被引:110
作者
Jiang Dabang
Wang Huijun
Lang Xianmei
机构
[1] Chinese Academy of Sciences,Nansen
[2] Chinese Academy of Sciences,Zhu International Research Center, Institute of Atmospheric Physics
关键词
coupled model; East Asian climatology; evaluation;
D O I
10.1007/BF02918482
中图分类号
学科分类号
摘要
Using observation and reanalysis data throughout 1961–1990, the East Asian surface air temperature, precipitation and sea level pressure climatology as simulated by seven fully coupled atmosphere-ocean models, namely CCSR/NIES, CGCM2, CSIRO-Mk2, ECHAM4/OPYC3, GFDL-R30, HadCM3, and NCAR-PCM, are systematically evaluated in this study. It is indicated that the above models can successfully reproduce the annual and seasonal surface air temperature and precipitation climatology in East Asia, with relatively good performance for boreal autumn and annual mean. The models’ ability to simulate surface air temperature is more reliable than precipitation. In addition, the models can dependably capture the geographical distribution pattern of annual, boreal winter, spring and autumn sea level pressure in East Asia. In contrast, relatively large simulation errors are displayed when simulated boreal summer sea level pressure is compared with reanalysis data in East Asia. It is revealed that the simulation errors for surface air temperature, precipitation and sea level pressure are generally large over and around the Tibetan Plateau. No individual model is best in every aspect. As a whole, the ECHAM4/OPYC3 and HadCM3 performances are much better, whereas the CGCM2 is relatively poorer in East Asia. Additionally, the seven-model ensemble mean usually shows a relatively high reliability.
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页码:479 / 495
页数:16
相关论文
共 81 条
[1]  
Cholaw Bueh(2003)The change of North China climate in transient simulations using the IPCC SRES A2 and B2 scenarios with a coupled atmosphere-ocean general circulation model Adv. Atmos. Sci. 20 755-766
[2]  
Cubasch U.(1999)Coupled ocean atmosphere model experiments of future climate change with an explicit representation of sulphate aerosol scattering J. Meteor. Soc. Japan 77 1299-1307
[3]  
Yonghui Lin(2001)Warming asymmetry in climate change simulations Geophys. Res. Lett. 28 195-198
[4]  
Liren Ji(1998)Simulation of the evolution of summer monsoon rainbelts over eastern China from regional climate model Chinese J. Atmos. Sci. 22 522-534
[5]  
Emori S.(2000)The simulation of SST, sea ice extents and ocean heat transports in a version of the Hadley Centre coupled model without flux adjustments Climate Dyn. 16 147-168
[6]  
Nozawa T.(1997)Transient climate change in the CSIRO coupled model with dynamic sea ice Mon. Wea. Rev. 125 875-907
[7]  
Abe-Ouchi A.(2003)Long-term climate variations in China and global warming signals J. Geophys. Res. 108 4614-4614
[8]  
Numaguti A.(2000)Impact of global warming on the Asian winter monsoon in a coupled GCM J. Geophys. Res. 105 4607-4624
[9]  
Kimoto M.(1994)Recent and future climate change in East Asia International Journal of Climatology 14 637-658
[10]  
Nakajima T.(2004)East Asian climate change trend under global warming background Chinese Journal of Geophysics 47 675-681