| 1 | The study of the Kuroshio in the East China Sea and the currents east of the Ryukyu Islands显示文摘In this study, the inverse method is used to compute the Kuroshio in the East China Sea and southeast of Kyushu and the currents east of the Ryukyu Islands, on the basis of hydrographic data obtained during September-October, 1987 by R/V Chofu Maru. The results show that: (1)A part of the Taiwan Warm Current has a tendency to converge to the shelf break; (2) the Kuroshio flows across the section C3 (PN) with a reduced current width, and the velocity of the Kuroshio at the section C3 increases and its maximum current speed is about 158 cm/s, and its volume transport here is about 26×106m3/s; (3) the Kuroshio has two current cores at the sections C3 (PN) and B2 (at the Tokara Strait); (4) the currents east of the Ryukyu Islands are found to flow northward over the Ryukyu Trench during September-October, 1987. The velocities of the currents are not strong throughout the depths. At the section C2 east of the Ryukyu Islands, the maximum current speed is at the 699 m levei and its magnitude is 25 cm/s, and | Yuan Yaochu, Endoh Masahiro and Ishizaki Hiroshi The Second Institute of Oceanography, State Oceanic Administration, Hangzhou, 310012, ChinaMeteorological Research Institute, JMA, Tsukuba 305, Japan | 1991 | Acta Oceanologica Sinica1991，10，3： | 7 |
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