To study seasonal variability in the Tsushima Warm Current, flowing to
the northeast in the Tsushima-Korea Strait, ADCP surveys were underta
ken about every 2 months from 1990 to 1991. The survey line extended f
rom Kawajiri-misaki, Japan, to some 30 km off Ulsan, Korea. The tidal
current component was removed from raw ADCP data to understand the reg
ional residual current. The total volume transport towards the northea
st, across the Strait, was at a maximum of 5.6 Sv (1 SV = 1 X 10(6) m3
s-1), in September. Total volume transports were around 1.0 Sv during
the other months. Seasonal variability in the current structure acros
s the Strait has also been investigated. The intensified core of the n
ortheasterly current formed near the Korean coast-in September. This r
esulted in the maximum total volume transport in the same month.