@article{oai:ir.kagoshima-u.ac.jp:00002328,
 author = {YUWAKI, Yasutaka and HIGASHI, Masataka and SHIMADA, Kiyoshi and HENMI, Tomio},
 issue = {1},
 journal = {鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University},
 month = {2016-10-27},
 note = {The sea surface temperature and the sea surface current were measured on board the Keiten
Maru every 6.3 miles along the round trip cruise between Kagoshima and Takamatu on May of
1987. The transition zone between the Kuroshio and the Seto Inland Sea waters was found in
the Bungo Channel. The sea surface temperature in the Kuroshio and the Seto Inland Sea were
20°-22°C and 15°C, respectively.
The horizontal gradient of temperature in the transition zone were about 0.12°C/mile on Leg
1 (outward cruise) and about 0.07°C/mile on Leg 2 (return cruise). The front was formed near
the western region of the Sea of Iyo (33°-30'.0 N, 132°-08'.0 E). In the Sea of Hyuga, when the
current direction is northward in the northern part, it is southward in the southern part, and
when it is southward in the northern part, it is northward in the southern part.},
 pages = {189--200},
 title = {Sea Surface Temperature and Surface Current in the East of Kyusyu and in the Seto Inland Sea on May of 1987},
 volume = {36},
 year = {}
}