対馬海流々域の水塊について

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  • On the Water Masses in the Tsushima Current Area
  • ツシマ カイリュウクリカエシイキ ノ スイカイ ニ ツイテ

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In this paper, the kinds, the formation and the mixing of the water masses in the Tsushima Current area are discussed by making use of the results of the oceanographical observations carried out until now. The outstanding features are as follows:<BR>1. The water, which passes the eastern canal of the Tsushima Strait, is the oceanic surface water mixed slightly with the coastal water of the East China Sea, and the one, which passes the western canal, is composed of the oceanic surface water mixed remarkably with the coastal water of the East China Sea and the western North Pacific central water indicated by SVERDRUP. The central water advances ascending toward the north-west along the bottom of the sea valley west off the Kyfishil district and flows into the Japan Sea.<BR>2. In the sea west off the Kyfishil district, lateral mixing is dominant between the oceanic water and the coastal water of the East China Sea.<BR>3. In the Japan Sea, sinking of surface water seems to lead the formation of the Japan Sea central water whose temperature-salinity curve is reflected to the temperature-salinity relation at the surface layer in late winter.<BR>4. The arrangement of the water masses in the Tsushima Current area of the Japan Sea in a vertical direction is considered to be such that the water which has flown into the Japan Sea from Tsushima Strait, the Japan Sea central water, the intermediate water and the deep water.

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