卢鋈,许鑑明. 1936. 中国夏季风暴之路径与其雨量之分布[J]. 气象学报, 12(8):307-408, doi:10.11676/qxxb1936.059
中国夏季风暴之路径与其雨量之分布
THE RAINFALL DISTRIBUTION OF THE SUMMER CYCLONES OF EASTERN CHINA(AN ABSTRACT)
  
DOI:10.11676/qxxb1936.059
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卢鋈  
许鑑明  
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中文摘要:
      作者为明瞭中国温带风暴及台风雨量分布之情形及其与路径之关系,特取民国二十四年夏季(六月至八月)经过中国本部之温带风暴及登陆之台风,逐一分别检讨。
英文摘要:
      Before the Mai-U or the plume rain season, the cyclones of Eastern China mostly travel far south of the Yangtze river in a direction from SW to NE. The distribution of rai fall is very even on both sides of the track. During the Mai-U period, the tracks of the cyclones move slightly northwards, but still keep to the south of the Yangtze. In this case the distribution of rainfall is asymmetrical and the rainfall belts are usually situated in the left hand quarters of the cyclones, or in the northern side of the tracks. This uneven distribution of rainfall is very striking as cn,npared with that of the cyclones before the Mai-U period. The rainfall belt is about 300 km in wideth The cyclones of North China are mostly rainless, except when they come near to the saa coast. But in their journey eastwards, after having travelled vast expanse of the Yellow Sea, they always cause heavy rain Kores and tha amount is even comparable with that of the cyclones of the Yangtze Valley.The rainafll belt is sometimes situated to the south and sometimes to the north of the track.
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