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《Chinese Journal of Geophysics》 2005-03
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Numerical modeling of interannual anomalous atmospheric circulation patterns over East Asia during different stages of an El Nino event

SUN Xu-Guang, YANG Xiu-Qun Institute of Severe Weather and Climate, Nanjing University, Nanjing 210093,China  
We make numerical modeling for the response of global atmosphere to the prescribed realistic monthly-varying global sea surface temperature during 1948~1999 with an atmospheric general circulation model (CCM3/NCAR). Then we analyze interannual anomalous atmospheric circulation patterns over East Asia during different stages of an El Nino cycle, with the SVD and composite analysis methods. The result shows that during the summer when an El Nino event develops, there exists an anomalously negative geopotential height center over Northeast China, the Korean peninsula and the Sea of Japan. The subtropical high over the western Pacific is weaker and shifts eastward, and East Asian summer monsoon is strengthened. During the winter when an El Nino event is matured, the East Asian trough is deepened, resulting in a strengthened winter monsoon over the north of East Asia but a weakened one over the south. During the summer when an El Nino event decays, the subtropical high over the western Pacific is stronger and shifts southward and westward, and the East Asian summer monsoon is weakened. There is a closest relationship between the El Nino event and atmospheric anomalies in East Asia only during the summer when the El Nino event decays. Overall, the simulated atmospheric anomaly patterns over East Asia due to El Nino's impact can reasonably explain the observed temperature and precipitation anomaly patterns that were described in previous studies.
【Fund】: 国家自然科学基金 (4 0 2 3 3 0 2 8);; 国家杰出青年科学基金 (4 0 42 5 0 0 9)资助
【CateGory Index】: P434
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