@article{oai:ir.kagoshima-u.ac.jp:00004826,
 author = {ICHIKAWA, Hiroshi and HIGASHIKAWA, Seiji and NISHI, Tooru and ARIMA, Sumihiro and MASUMITSU, Sunao and UCHIYAMA, Masaki},
 issue = {1},
 journal = {鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University},
 month = {2016-10-28},
 note = {Intensive oceanographic survey was carried out on Sept. 12 and 13 of 1984 in the region east
of Kyushu. The CTD observations were made at 14 stations on the two parallel sections ESE
of Hyuga and Nobeoka, ca 10 miles apart to each other. In addition, at 29 stations in a small
triangular area in this region, the XBT observations were made. The distances of two
adjacent CTD stations are mainly ca 5 miles and XBT ca 1 or 2 miles. The preliminary
results are as follows.
Was found the down intrusion of less saline surface water to a depth of 30 m layer of a point ca
10 miles apart. The isolated saline water was detected on the subsurface layer near the
coast. The geostrophic calculation refered to 1000 dbar revealed the existence of coastal
counter current with the maximum SSW component of 55 cm/sec. The width of this counter
current is more than 30 miles off Nobeoka (nouthern section) and less than 15 miles off Hyuga
(southern section). The XBT results show that the widths of small scale cold cores and warm
tongues are in the order of two miles.},
 pages = {151--168},
 title = {The Oceanic Condition in the Region East of Kyushu I : Intensive Survey in September of 1984},
 volume = {34},
 year = {}
}