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《Chinese Journal of Atmospheric Sciences》 2005-05
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The Structure and Activity Characteristics of the Western Pacific Subtropical Anticyclone and Its Dynamical Mechanism During the Meiyu Period over the Huaihe River Basin in 2003

ZHAO Bing-Ke~1, 2, YAO Xiu-Ping~1, 3, and WU Guo-Xiong~11 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 2 Graduate School of the Chinese Academy of Sciences, Beijing 100039 3 China Meteorological Administration Training Center, Beijing 100081  
The routine NCEP/NCAR reanalysis data were used for analyzing the characteristics of the western Pacific subtropical anticyclone (WPSA) during the Meiyu period in 2003. It is found that the WPSA is characterized by northward and stable relative to that of the climate mean, as well as the obvious east-west oscillation. The northward moving of the WPSA is prevented by the strong and stable western jet in mid-latitudes, thus causes the stable rainband over the Huaihe River basin. Meanwhile, the results show that the occurrence of each torrential rain is almost accompanied by the eastward moving of the South Asia high in upper-layer, and the westward extension of the 500 hPa WPSA to west coast of China. As a result, the high temperature and drought occur over the south of the Yangtze River. The possible mechanisms of the subtropical anticyclone in the higher and lower layer triggering the development of the weather system are summarized as follows: (1) The ridge of the eastward South Asia high along 30°N causes the divergence and ascent motion to the north of 30°N while the convergence and descending motion to the south of 30°N over the Huaihe River basin. (2) The divergence of the convergence and descending airflow further enhances the local negative vorticity in the lower layer, which leads to the westward extending of the WPSA. (3) The convergence of the southwesterly to the north of 30°N along the northwest of the WPSA strengthens the local ascending motion, which provides a large-scale background favorable for the torrential rain. (4) The torrential rain to the northwest of the WPSA intensifies the southerly in the lower layer and the northerly in the higher layer, and it makes the eastward South Asia high and the WPSA stably maintain over the area.
【Fund】: 国家自然科学基金资助项目40135020、40375022和40205008
【CateGory Index】: P461.2
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