蒋尚城,张镡,周鸣盛,刘盎然. 1981. 登陆北上减弱的台风所导致的暴雨——半热带系统暴雨[J]. 气象学报, 39(1):18-27, doi:10.11676/qxxb1981.003 |
登陆北上减弱的台风所导致的暴雨——半热带系统暴雨 |
THE HARD RAINSTORMS IN NORTH CHINA INDUCED BY A LANDED NORTHWARD MOVING AND DECAYING TYPHOON——HARD RAINSTORMS OF SEMI-TROPICAL SYSTEMS |
投稿时间:1979-09-25 修订日期:1980-02-09 |
DOI:10.11676/qxxb1981.003 |
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中文摘要: |
分析了登陆北上减弱的78051)号台风在华北所产生的暴雨过程。指出:在中低纬系统相互作用下,导致暴雨的系统具有半热带性质。讨论了半热带气旋和半热带锋区的特征,并比较了大陆半热带气旋与海洋半热带气旋的不同,强调进一步研究半热带天气系统是重要的。 |
英文摘要: |
In this paper, hardstorm rainfall processes in north-China induced by a landed northward moving and decaying typhoon axe analysised. It is shown that under the interaction between synoptic systems of the mid- and low-latitude belts, the hard rainfall bearing systems possess semi-tropical characteristic. The characteristics of the semi-tropical cyclone and semi-tropical front are discussed and the difference between the continental and oceanic semi-tropical cyclones is pointed out. Finally, it is emphasized that futher studies of semi-tropical synoptic systems are of great significance. |
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