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The correctness to the spuriously simulated semi-annual cycle of the sea surface temperature in the equatorial eastern Pacific

The correctness to the spuriously simulated semi-annual cycle of the sea surface temperature in the equatorial eastern Pacific

作     者:SONG ZhenYa QIAO FangLi WANG ChunZai 

作者机构:The First Institute of Oceanography State Oceanic Administration Qingdao 266061 China NOAA Atlantic Oceanographic and Meteorological Laboratory Miami USA 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2011年第54卷第3期

页      面:438-444页

核心收录:

学科分类:0711[理学-系统科学] 07[理学] 070601[理学-气象学] 0708[理学-地球物理学] 0706[理学-大气科学] 0704[理学-天文学] 

基  金:supported by National Natural Science Foundation of China (Nos. 40730842 and 40906018) 

主  题:赤道东太平洋 逻辑模拟 温度循环 海洋表面温度 国家重点实验室 气候模型 海面 耦合理论 

摘      要:One of the challenges faced by the climate model of the Community Climate System Model version 3 (CCSM3) is the spuriously simulated semi-annual cycle of the sea surface temperature (SST) in the equatorial eastern Pacific. This model bias has limited the performance of the climate simulation and prediction. Based on the surface wave-circulation coupled theory, an atmosphere-wave-ocean coupled model was developed, which incorporates the MASNUM (key laboratory of Marine Sciences and Numerical Modeling) wave number spectral model into CCSM3. The new coupled atmosphere-wave-ocean model successfully removes the spurious semi-annual cycle simulated by the original CCSM3 and reasonably produces an SST annual cycle with warm and cold phases in April and August, respectively. The correlation between the simulated and observed SST in the equatorial eastern Pacific is improved from 0.66 to 0.93. The ocean surface layer heat budget analysis indicates that the wave-induced vertical mixing is responsible for improving the simulation of the SST seasonal cycle in the equatorial eastern Pacific.

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