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| SOUTHWEST MONSOON SURGE AND ITS WEATHER IMPACT | |
| 作者姓名： | 方翔 郑新江 朱福康 李云 李曾中 |
| 作者单位： | School of Physics Peking University，National Satellite Meteorological Center CMA，Beijing 100081 China Beijing 100081 China，Guangzhou Institute of Tropical and Marine Meteorology CMA，National Satellite Meteorological Center CMA，Beijing 100081 China Beijing 100081 China，Chinese Academy of Meteorological Sciences，National Satellite Meteorological Center CMA，Beijing 100081 China，Chinese Academy of Meteorological Sciences，Beijing 100871 China，Guangzhou 510080 China，Beijing 100081 China，Beijing 100081 China，Beijing 100081 China |
| 基金项目： | 国家重点基础研究发展计划(973计划) |
| 摘 要： | The sustained rainfall process on May 13-22, 2004 was one of the pre-summer rainy periods in the south of China. It was related with the genesis and development of a SW monsoon surge over the Bay of Bengal. From the synoptic analysis it is found that the genesis and development of the SW monsoon surge may be divided approximately into the initial, developing and decaying stages. During the rainfall the Southern Hemisphere cross-equatorial flow over the Indian Ocean plays a triggering role. |
| 关 键 词： | 下雨周期 中国 季风 赤道 |
SOUTHWEST MONSOON SURGE AND ITS WEATHER IMPACT |
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| FANG-Xiang,ZHENG Xin-jiang,ZHU Fu-kang,LI Yun,LI Zeng-zhong.SOUTHWEST MONSOON SURGE AND ITS WEATHER IMPACT[J].Journal of Tropical Meteorology,2007,13(1):41-44. | |
| Authors: | FANG-Xiang ZHENG Xin-jiang ZHU Fu-kang LI Yun LI Zeng-zhong |
| Institution: | 1. School of Physics, Peking University, Beijing 100871 China;National Satellite Meteorological Center, CMA, Beijing 100081 China, Beijing 100081 China 2. Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080 China;National Satellite Meteorological Center, CMA, Beijing 100081 China, Beijing 100081 China 3. Chinese Academy of Meteorological Sciences, Beijing 100081 China 4. National Satellite Meteorological Center, CMA, Beijing 100081 China, Beijing 100081 China |
| Abstract: | The sustained rainfall process on May 13-22, 2004 was one of the pre-summer rainy periods in the south of China. It was related with the genesis and development of a SW monsoon surge over the Bay of Bengal. From the synoptic analysis it is found that the genesis and development of the SW monsoon surge may be divided approximately into the initial, developing and decaying stages. During the rainfall the Southern Hemisphere cross-equatorial flow over the Indian Ocean plays a triggering role. |
| Keywords: | yearly-first rainy period in South China SW monsoon surge cross-equatorial flow |
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