@article{oai:ir.kagoshima-u.ac.jp:00010898,
 author = {TAKAHASHI, Tadao and CHAEN, Masaaki and UEDA, Soichi},
 journal = {鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University},
 month = {2016-10-31},
 note = {The general informations obtained from the Kagoshima-maru IGY cruise, 1958, in the
western Equatorial Pacific are presented. A cold water of 10°C climbs up to ca 250m depth
at ca 5°N. Temperature of the core of salinity maximum of higher than 35% extending to
the north from the southern latitudes in a layer around 150m depth is ca 23°C. Low salinity
is found around 5°N. Oxygen content in a layer above 100m is ca 4cc/l and below the layer
the vertical gradient is strong to the north of 3°N. The South Equatorial Current is found
in a region to the south of 2°N and below the Current an eastward flow exists. It is difficult
to distinguish the Equatorial Undercurrent from the Equatorial Countercurrent flowing
eastwards in a region to the north of the South Equatorial Current. The amount of the
eastward volume transport above a depth of 400m, based on direct measurement, is ca 93
million m^3/sec and that of westward is ca 25 million m^3/sec.},
 pages = {82--86},
 title = {Report of the Kagoshima-maru IGY Cruise, 1958},
 volume = {8},
 year = {}
}