| 梅雨期盛期的大尺度涡度收支特征 |
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| 引用本文： | 汪钟兴.梅雨期盛期的大尺度涡度收支特征[J].热带气象学报,1986,0(3):211-217. |
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| 作者姓名： | 汪钟兴 |
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| 作者单位： | 中国科技大学 |
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| 摘 要： | 本文计算了1983年长江中下游梅雨期盛期的大尺度涡度收支,并分别给出收支方程各项的水平和垂直分布。结果表明,雨区附近的对流层上、下层均有大范围显著的余差存在,它意味着积云对流在涡度平衡中起着重要作用。
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| 收稿时间： | 1985/10/22 0:00:00 |
| 修稿时间： | 1986/1/18 0:00:00 |
THE FEATURE OF THE LARGE-SCALE VORTICITY BUDGET DURING THE MID MEI-YU SEASON |
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| Wang Zhongxing.THE FEATURE OF THE LARGE-SCALE VORTICITY BUDGET DURING THE MID MEI-YU SEASON[J].Journal of Tropical Meteorology,1986,0(3):211-217. |
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| Authors: | Wang Zhongxing |
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| Institution: | University of Science and Technology of China |
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| Abstract: | In this paper we calculated the large-scale vorticity budget during the mid MEI-YU season of 1983 and presented the mean horizontal pattern and vertical profile of budget equation terms. The significant residual near precipitation tegion was found to exist in the upper and lower troposphere. This result implies that convective scale motion exert an important effect on the vorticity balance. |
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