Abstract
The path of the Kuroshio in Sagami Bay was surveyed through drifter tracking from Oshima-West Channel to Oshima-East Channel. A subsurface drifter with a drogue at 300 m depth flowed around Oshima from Oshima-West Channel to Oshima-East Channel. A difference in flow directions between the upper and lower layers was apparent in the northwest of Oshima. Flow directions there were shown to change from north in the surface layer to east in the bottom layer, and this was confirmed with moored currentmeters.
A profile of northward current velocity was estimated from measurements in six layers with currentmeters deployed in the Oshima-West Channel. The profile shows a core of northward flow along the eastern bottom slope and a weak southward flow along the western bottom slope. Volume transport of the Kuroshio into Sagami Bay was estimated to be 1.8×106m3sec−1 from the profile.
Long-term current measurement showed that southward flows were observed in Oshima-West Channel in July 1977, May 1978 and April 1979. Cold or warm water masses appearing south of the Izu Peninsula are suggested to have caused the changes.
Displacement of the cold water mass in July 1977 is discussed on the basis of current measurements and offshore oceanographic conditions.
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Taira, K., Teramoto, T. Path and volume transport of the Kuroshio current in Sagami Bay and their relationship to cold water masses near Izu Peninsula. Journal of the Oceanographical Society of Japan 42, 212–223 (1986). https://doi.org/10.1007/BF02109355
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DOI: https://doi.org/10.1007/BF02109355