Seasonal and intraseasonal variations of East Asian summer monsoon precipitation simulated by a regional air-sea coupled model

被引:14
作者
Fang Yongjie [1 ]
Zhang Yaocun [2 ]
Huang Anning [2 ]
Li Bo [3 ]
机构
[1] China Meteorol Adm, Beijing Climate Ctr, Beijing 100081, Peoples R China
[2] Nanjing Univ, Sch Atmospher Sci, Nanjing 210093, Jiangsu, Peoples R China
[3] China Meteorol Adm, Key Lab Radiometr Calibrat & Validat Environm Sat, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
regional air-sea coupled model; East Asian summer monsoon rainfall; climatological intraseasonal oscillation; CLIMATE MODEL; PART I; RAINFALL; CHINA; TEMPERATURE; CIRCULATION; PERFORMANCE; IMPACT;
D O I
10.1007/s00376-012-1241-6
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The performance of a regional air-sea coupled model, comprising the Regional Integrated Environment Model System (RIEMS) and the Princeton Ocean Model (POM), in simulating the seasonal and intraseasonal variations of East Asian summer monsoon (EASM) rainfall was investigated. Through comparisons of the model results among the coupled model, the uncoupled RIEMS, and observations, the impact of air-sea coupling on simulating the EASM was also evaluated. Results showed that the regional air-sea coupled climate model performed better in simulating the spatial pattern of the precipitation climatology and produced more realistic variations of the EASM rainfall in terms of its amplitude and principal EOF modes. The coupled model also showed greater skill than the uncoupled RIEMS in reproducing the principal features of climatological intraseasonal oscillation (CISO) of EASM rainfall, including its dominant period, intensity, and northward propagation. Further analysis indicated that the improvements in the simulation of the EASM rainfall climatology and its seasonal variation in the coupled model were due to better simulation of the western North Pacific Subtropical High, while the improvements of CISO simulation were owing to the realistic phase relationship between the intraseasonal convection and the underlying SST resulting from the air-sea coupling.
引用
收藏
页码:315 / 329
页数:15
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