Abstract
Mean flows and velocity fluctuations are described from direct measurements of bottom currents made at three stations across Nankai Trough and two stations in Sagami Trough from May 1982 to May 1984. Aanderaa current meters were moored 7 m above the bottom. The observed mean flows indicate a counter-clockwise circulation in Nankai Trough with current speeds of 0.9–2.1 cm sec−1. The mean flows were larger on the slopes than on the flat bottom of the trough. The mean flows observed in Sagami Trough show an inflow into Sagami Bay which is considered to be a part of the Oyashio undercurrent from the north that flows along the eastern coast of Honshu. Velocity fluctuations with periods greater than 100 hr were less energetic in the troughs than those at a station west of Hachijo-jima Island. A highly energetic fluctuation with a period of 66.7 hr was observed on the northern slope of Sagami Trough in the velocity component parallel to the trough axis. A maximum current speed of 49 cm sec−1 was observed in Sagami Trough.
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This study was sponsored by the Ministry of Education, Science and Culture, Japan.
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Taira, K., Teramoto, T. Bottom currents in Nankai Trough and Sagami Trough. Journal of the Oceanographical Society of Japan 41, 388–398 (1985). https://doi.org/10.1007/BF02109033
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DOI: https://doi.org/10.1007/BF02109033