大气科学进展(英文版)
大氣科學進展(英文版)
대기과학진전(영문판)
ADVANCES IN ATMOSPHERIC SCIENCES
2010年
5期
1131-1142
,共12页
包庆%吴国雄%刘屹岷%杨静%王在志%周天军
包慶%吳國雄%劉屹岷%楊靜%王在誌%週天軍
포경%오국웅%류흘민%양정%왕재지%주천군
东亚夏季风%耦合模式%大气物理研究所%国家重点实验室%数值模拟%性能%表面温度分布%地球物理
東亞夏季風%耦閤模式%大氣物理研究所%國傢重點實驗室%數值模擬%性能%錶麵溫度分佈%地毬物理
동아하계풍%우합모식%대기물리연구소%국가중점실험실%수치모의%성능%표면온도분포%지구물리
East Asian Summer Monsoon%ocean–atmosphere–land model%climatological mean state%in-terannual variability%ENSO
The spectral version 1.1 of the Flexible Global Ocean–atmosphere–land System (FGOALS1.1-s) model was developed in the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophys- ical Fluid Dynamics at the Institute of Atmospheric Physics (LASG/IAP). This paper reports the major modifications to the physical parameterization package in its atmospheric component, including the radiation scheme, convection scheme, and cloud scheme. Furthermore, the simulation of the East Asian Summer Monsoon (EASM) by FGOALS1.1-s is examined, both in terms of climatological mean state and interannual variability.
The results indicate that FGOALS1.1-s exhibits significant improvements in the simulation of the balance of energy at the top of the atmosphere: the net radiative energy flux at the top was 0.003 W m-2 in the 40 years fully coupled integration. The distribution of simulated sea surface temperature was also quite reasonable, without obvious climate drift. FGOALS1.1-s is also capable of capturing the major features of the climatological mean state of the EASM: major rainfall maximum centers, the annual cycle of precipitation, and the lower-level monsoon circulation flow were highly consistent with observations in the EASM region.
Regarding interannual variability, simulation of the EASM leading patterns and their relationship with sea surface temperature was examined. The results show that FGOALS1.1-s can reproduce the first leading pattern of the EASM and its close relationship with the decaying phase of the ENSO. However, the model lacked the ability to capture either the second major mode of the EASM or its relationship with the developing phase of the ENSO.