中國東岸沿海風信力學的意義及其對於温度的影響

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。在這兩個區域内,等温線的分布,格外特别。如黃海西區,等温線在山東半島南部向陸地突入,經東海徐州成一舌狀。

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

In the north of Shantung Peninsula, moderate northerly cwrrent becoms deflected by the peninsula towatd the east end, then turns South- ward. Dynanically a vortex motion is thus formed over the west of Yellow Sea and south of the Peninsula, a evidenced from the annual prevailing winds around the Yellow Sea (Fig. 6). The eirclmstance to form a perfest vortex motion, even in winter seems rare; but from the distributions of temperature and rainfall over east and west hilly regions as well as over the south and...