1996
DOI: 10.1007/bf02236534
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Downstream transition of the Tsushima Current west of Kyushu in summer

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Cited by 26 publications
(13 citation statements)
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“…Some reports indicate the existence of a clockwise current near Kyusyu Island (e.g., Lie & Cho 2002;Katoh et al 2004); this clockwise current was considered a branch of the Tsushima Current in their schematic circulation maps (Lie & Cho 2002;Katoh et al 2004). Katoh et al (1996) clarified the current structures in this area and observed the clockwise bifurcation of the Tsushima Current that flows southward near the west coast of Goto Islands in July and September 1990, although it is unclear whether the bifurcation occurs steadily or intermittently. Nakamura et al (1988) observed the east-southeast flow of the current at a depth of 50 m in the middle area near the continental shelf edge, south off Goto Islands from July to September in 1985.…”
Section: Surface Driftersmentioning
confidence: 96%
“…Some reports indicate the existence of a clockwise current near Kyusyu Island (e.g., Lie & Cho 2002;Katoh et al 2004); this clockwise current was considered a branch of the Tsushima Current in their schematic circulation maps (Lie & Cho 2002;Katoh et al 2004). Katoh et al (1996) clarified the current structures in this area and observed the clockwise bifurcation of the Tsushima Current that flows southward near the west coast of Goto Islands in July and September 1990, although it is unclear whether the bifurcation occurs steadily or intermittently. Nakamura et al (1988) observed the east-southeast flow of the current at a depth of 50 m in the middle area near the continental shelf edge, south off Goto Islands from July to September in 1985.…”
Section: Surface Driftersmentioning
confidence: 96%
“…Shortterm current observations have shown strong currents with large tidal components (Mizuno et al, 1989;Egawa et al, 1993;Isobe et al, 1994;Katoh et al, 1996) and are thought to be dominated by large seasonal variability (Yi, 1970;Kawabe, 1982;Toba et al, 1982;Egawa et al, 1993). These studies suggest currents are at a maximum in summer through fall and are at a minimum in winter through spring in the west channel.…”
mentioning
confidence: 92%
“…Kyushu Island on the western coast of Japan (Fig. 1) is located on the margin of the East China Sea (ECS), and the hydrodynamic environment is strongly influenced by the Kuroshio Current and the Tsushima Warm Current (Katoh et al, 1996). Because the Kuroshio Current and the Tsushima Warm Current transport larvae and juveniles of many fish species from southern spawning grounds to the waters off western Kyushu Island (e.g., Sassa et al, 2006;Okazaki and Nakata, 2007;Kitagawa et al, 2010).…”
Section: Introductionmentioning
confidence: 99%