| 初夏东亚大尺度低空强西风分支的数值模拟 |
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| 引用本文： | 田永祥,尹树新,钱盛光,张迎新.初夏东亚大尺度低空强西风分支的数值模拟[J].热带气象学报,1989(4):305-313. |
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| 作者姓名： | 田永祥 尹树新 钱盛光 张迎新 |
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| 作者单位： | 南京气象学院
(田永祥，尹树新，钱盛光)，南京气象学院(张迎新) |
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| 摘 要： | 本文采用p—σ坐标五层原始方程模式模拟出初夏东亚大尺度低空强西风分支的现象.并进一步阐明低空强西风分支及其对应的副热带季风雨带和热带季风雨带形成的物理机制,本文所得的结果对于初夏长江中下游流域的梅雨和南海海域的降水预报有一定参考价值
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| 收稿时间： | 9/1/1988 12:00:00 AM |
| 修稿时间： | 1988/11/24 0:00:00 |
THE NUMERICAL SIMULATION OF THE BIFURCATION OF THE STRONG LARGE SCALE LOW-LEVEL WESTERLY IN EAST ASIA IN EARLY SUMMER |
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| Tian Yongxiang,Yin Shuxin,Qian Shengguang and Zhang Yingxin.THE NUMERICAL SIMULATION OF THE BIFURCATION OF THE STRONG LARGE SCALE LOW-LEVEL WESTERLY IN EAST ASIA IN EARLY SUMMER[J].Journal of Tropical Meteorology,1989(4):305-313. |
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| Authors: | Tian Yongxiang Yin Shuxin Qian Shengguang and Zhang Yingxin |
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| Institution: | Nanjing Instiute of Meteorology;Nanjing Instiute of Meteorology;Nanjing Instiute of Meteorology;Nanjing Instiute of Meteorology |
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| Abstract: | The phenomenon of the bifurcation of the strong large scale low-level westerly in East Asia in early summer is simulated with a five-layer primitive equations model. The physical mechanism for forming the bifurcation of the strong low-level westerly and the corresponding subtropical monsoon rain belt and tropical monsoon rain belt is explained further. The simulated results will be beneficial to the forecasting of the Mei-Yu in the middle-lower reaches of the Yangtze River and precipitation in the South China Sea Waters. |
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