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《Chinese Journal of Atmospheric Sciences》 2004-01
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A Simulation of Regional Climate in China by Using CCM3 and Observed SST

Gao Xuejie 1), Lin Wantao 2), Fred Kucharsky 3), and Zhao Zongci 1)1) (National Climate Center, China Meteorological Administration, Beijing 100081) 2) (Institute of Atmospheric physics, Chinese Academy of Sciences, Beijing 100029) 3) (The Abdus Salam International Center for Theoretical Physics, Trieste, Italy)  
Driven by observed SST and sea ice, 5 ensemble AMIP2 runs for 19 years (1979~1997) were conducted by NCAR/CCM3. Results of the runs in China focused on air surface temperature and precipitation were analyzed. It shows that the model can reproduce well the annual mean air surface temperature pattern in China. However the simulated temperature exhibites a general cold bias of a few degrees over extended regions while the bias may be even greater in the regions with the fine topography. The model fails in the simulation of precipitation. It tends to simulate a virtual big precipitation center in mid China, as the other GCMs did. Analysis of the simulated summer precipitation anomaly shows that the model has a generally poor ability in its simulation in China, but it does show the ability in some regions, e.g. Yangtze River valley. The model has a better performance to simulate the summer temperature anomaly, especially in eastern part of North China.
【Fund】: 国家杰出青年基金 40 1 2 5 0 1 4;; 中国气象局IPCC专项经费资助
【CateGory Index】: P461
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