An introduction to the coupled model FGOALS1.1-s and its performance in East Asia

被引:61
作者
Bao Qing [1 ]
Wu Guoxiong [1 ]
Liu Yimin [1 ]
Yang Jing [2 ]
Wang Zaizhi [3 ]
Zhou Tianjun [1 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[2] Beijing Normal Univ, ESPRE, Beijing 100875, Peoples R China
[3] China Meteorol Adm, Beijing Climate Ctr, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
East Asian Summer Monsoon; ocean-atmosphere-land model; climatological mean state; interannual variability; ENSO; GENERAL-CIRCULATION MODELS; INTERANNUAL VARIABILITY; AUSTRALIAN MONSOON; TROPICAL PACIFIC; LEADING MODES; CLIMATE; ATMOSPHERE; PARAMETERIZATION; PARAMETRIZATION; LASG/IAP;
D O I
10.1007/s00376-010-9177-1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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 Geophysical 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 EASMor its relationship with the developing phase of the ENSO.
引用
收藏
页码:1131 / 1142
页数:12
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