涂长望, 郭晓岚. 1938: Koeppen范式的中国气候区域. 气象学报, (2): 51-67. DOI: 10.11676/qxxb1938.005
引用本文: 涂长望, 郭晓岚. 1938: Koeppen范式的中国气候区域. 气象学报, (2): 51-67. DOI: 10.11676/qxxb1938.005
TU CHANG-WANG, SHIAO-LAN KUO. 1938: Climatic Regions of China According to Koeppen’s Classification. Acta Meteorologica Sinica, (2): 51-67. DOI: 10.11676/qxxb1938.005
Citation: TU CHANG-WANG, SHIAO-LAN KUO. 1938: Climatic Regions of China According to Koeppen’s Classification. Acta Meteorologica Sinica, (2): 51-67. DOI: 10.11676/qxxb1938.005

Koeppen范式的中国气候区域

Climatic Regions of China According to Koeppen’s Classification

  • 摘要: 著者在其『中国气候区域』一文中已详论过中国的气候及其分划,(气象研究所集刊第八号)但其目的纯为适应中国的需要和实用;对於不明瞭中国地理环境及名称的人则显得生疏而不易捉摸。为易於与世界其他各处的气候性质相比较及供不熟悉中国地名的人们的需要起见,爰乃根据Koeppen氏的分类法将中国气候重新划分。

     

    Abstract: An attempt has been made to classify the climatic regions of China according to Koeppen's 6nodified crieria and it is found that the new map differs notably from Koeppen's old map and the main differences are: 1.The BWkw region contains a much bigger area thin Koeppen's map; 2. the loess highlands are classifted as BSkw instead of Dwa in Koeppea's map; 3: the Cfa region constitutes a much bigger area than before, 4. the mountainous regions of western Szechuen, Sikang and Tibetan borderland should be classified as Dw instead cf Df. Furthermore the main climatic regions are subdivided into minor regions and the authors have introduced the product of mean annual rainfall and annual temperature to subdivide some of the major regions where Koeapen's criterion is not available.

     

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