| 初夏季风低槽活动与华南降水 |
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| 引用本文： | 王荫桐,彭洪.初夏季风低槽活动与华南降水[J].热带气象学报,1985(4):340-349. |
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| 作者姓名： | 王荫桐 彭洪 |
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| 作者单位： | 广东省热带海洋气象研究所
(王荫桐)，广东省热带海洋气象研究所(彭洪) |
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| 摘 要： | 通过对1971—1980年4—6月十年资料的普查分析,我们将华南季风低槽分为大陆(华南)和海域(南海)两类。前者发生在初夏前期,它与冬、夏季风有密切关系,是华南前汛期强降水的主要系统;后者与热带辐合带及孟加拉湾季风槽东伸至南海部分相联系,此类槽出现频数不多,但对南海及华南的影响也是非常重要的。
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| 收稿时间： | 1985/2/24 0:00:00 |
| 修稿时间： | 1985/6/24 0:00:00 |
THE RELATIONSHIP BETWEEN MONSOON TROUGH AND PRECIPITATION IN SOUTH CHINA DURING EARLY SUMMER |
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| Wang Yintong and Peng Hong.THE RELATIONSHIP BETWEEN MONSOON TROUGH AND PRECIPITATION IN SOUTH CHINA DURING EARLY SUMMER[J].Journal of Tropical Meteorology,1985(4):340-349. |
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| Authors: | Wang Yintong and Peng Hong |
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| Institution: | Guangdong Institute of Tropical Marine Meteorology;Guangdong Institute of Tropical Marine Meteorology |
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| Abstract: | In this paper , the monsoon trough in South China for ten years ( 1971-1980 ) are examined" and analysed. According to analysis, the monsoon trough are divided into two groups, one is in the land , this kind of monsoon trough occures on the border between the winter and the summer monsoons It is an important weather system during the previous rainy season in South China. The other is over the South China Sea and is related with ITCZ and monsoon trough over the Bay of Bengal. Its occurrence is not too frequent but it has serious influence on the area of South China. |
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