卢鋈. 1936: 中国之寒潮. 气象学报, (12): 651-679. DOI: 10.11676/qxxb1936.086
引用本文: 卢鋈. 1936: 中国之寒潮. 气象学报, (12): 651-679. DOI: 10.11676/qxxb1936.086
A. Lu. 1936: THE COLD WAVES OF CHINA. Acta Meteorologica Sinica, (12): 651-679. DOI: 10.11676/qxxb1936.086
Citation: A. Lu. 1936: THE COLD WAVES OF CHINA. Acta Meteorologica Sinica, (12): 651-679. DOI: 10.11676/qxxb1936.086

中国之寒潮

THE COLD WAVES OF CHINA

  • 摘要: 绪言(1)寒潮之行径(5)寒潮与天气(2)寒潮之各月分配附录一冬季之寒潮(3)寒潮大高空观测附录二初春之寒潮(4)寒潮与高低气压之关系附录三暮春之潮寒寒潮一名,乃专指北地冷气团南下时所生之诸种现象也。冷气团排除暖气团而代领其位,冷面於焉形成。其所经之地,温度低降,湿度锐减,气压增高,狂飚倏发,雨雹并施,雷电交作。天地为之震撼,草木因以零落。

     

    Abstract: Abstract. The cold waves of China are discussed under the following five headings: 1. The tracks of cold waves. It is found that the tracks of cold waves are closely related with the geographical features, and on the main they av oid the mountains and plateaux and follow the open plains and richer valleys. The velocity of travel is greatest when passing through a wind-gap or a narrow valley. 2. The monthly distribution of cold waves. Cold wave invasions begin earnestly in the month of October and last right until the next 1VYay. November and December have the greatest frequencies of cold wave burst.

     

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