抄録
Using the occupied area in the fixed section by the oceanic current, we can represent to some extent the intensity of the Kurosiwo and the Oyasiwo. In the present paper, we can see that the Kurosiwo was very strong in 1948, and it was a little warmer in 1949 than the average year, and the Kurosiwo and the Oyasiwo were both strong from spring to early summer in 1950.
