Abstract
In spring the water temperature innarrow straits in the Inland Sea indicates vertical homotherm distribution and relatively low value due to the turbulent mixing by strong tidal current, and is feasible to cause the dense fog, especially in the warm sector of cyclone with the consequent sea-disaster such as the case of "Shiun-Maru" (May 11, 1955). In the NE sea-district of Japan the most freguent occurrence of sea fog lies in the area of cold curent. In spite of the difficulty of searching, the whalers find the great concentration of whales at the head of the cold current where dense fog occurs most freguently. (See Fig.1 a〜f)
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