吕炯. 1941: 中國東岸沿海風信力學的意義及其對於温度的影響. 气象学报, (1): 3-26. DOI: 10.11676/qxxb1941.001
引用本文: 吕炯. 1941: 中國東岸沿海風信力學的意義及其對於温度的影響. 气象学报, (1): 3-26. DOI: 10.11676/qxxb1941.001
John Lee. 1941: Dynamical Effect of Eastern Chinese Coastal Winds and Its Influence upon the Temperature. Acta Meteorologica Sinica, (1): 3-26. DOI: 10.11676/qxxb1941.001
Citation: John Lee. 1941: Dynamical Effect of Eastern Chinese Coastal Winds and Its Influence upon the Temperature. Acta Meteorologica Sinica, (1): 3-26. DOI: 10.11676/qxxb1941.001

中國東岸沿海風信力學的意義及其對於温度的影響

Dynamical Effect of Eastern Chinese Coastal Winds and Its Influence upon the Temperature

  • 摘要: 我寫這篇文章的動機是由於繪製中國之温度圖而起,當我作温度圖時.發现一個特殊的現象,就是中國東部沿海岸及以島嶼上的温度,常是比較兩旁的温度為低.就是說比左邊的大陸和右邊的大洋,温度統要低些,這可拿年平均温度來代表(第一圖).這種現象在中國東岸有兩個區域特别顯著,一個是山東半島東端和江蘇北部的東海徐州一带,一個是在台灣海峽内.我們名上述兩個區域,一個為黃海西區一,個為台灣海峽區.

     

    Abstract: In the north of Shantung Peninsula,moderate northerly current becoms deflected by the penisala toward the east end,then tarns Southward.Dynamically a vortex motion is thus formed over the west of Yellow Sea and south of the Peninsula,as ovidenced from the annual prevailing winds around the Yellow Sea(Fig.6).

     

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