REFERENCES
Fujita. K. (1997): Study on the relation between the variation of the Kuroshio path south of Japan and the sea level difference between Kushimoto and Uragami. Dr. Thesis, Faculty of Bioresources, Mie Univ., 136 pp. (in Japanese).
Fujita. K., S. Yoshida and Y. Nagata (1998): Does small-scale meander travel eastwards and trigger Large-scale Meander of the Kuroshio. Acta Oceanographica Taiwanica, 37, 127-138.
Kawabe, M. (1980): Sea level variation along the south coast of Japan and the large meander in the Kuroshio. J. Oceanogr. Soc. Japan, 36, 97-104.
Masuzawa, J. (1965): Meanders of the Kuroshio. Kagaku, 35, 588-593 (in Japanese).
Nagata, Y., K. Fujita and S. Yoshida (1999a): Small-scale meander as a trigger of the Kuroshio Large Meander. La mer, 36, 119-130 (in Japanese).
Nagata, Y., J. Takeuchi, M. Uchida. I. Ishikura, Y. Morikawa and T. Koike (1999b): Current nature of the Kuroshio in the vicinity of the Kii Peninsula. J. Oceanogr., 55, 407-416.
Sekine, Y. and K. Fujita ( 1999): Why does the sea level difference between Kushimoto and Uragami show periods of large meander and non-large meander paths of the Kuroshio south of Japan? J. Oceanogr., 55, 43-51 .
Shoji, D. (1972): Time variation of the Kuroshio south of Japan. In Kuroshio―Its Physical Aspects―, ed. by H. Stommel and K. Yoshida, Univ. of Tokyo Press, pp. 217-234.
Taft, B. A. (1972): Characteristics of the flow of the Kuroshio south of Japan. In Kuroshio―Its Physical Aspects―, ed. by H. Stommel and K. Yoshida, Univ. of Tokyo Press, pp. 165-216.
Takeuchi, J., N. Honda, Y. Morikawa, T. Koike and Y. Nagata (1998a): Bifurcation Current along the southwest coast of the Kii Peninsula. J. Oceanogr., 54, 45-52.
Takeuchi, J., Y. Morikawa, I. Ishikura, M. Uchida, T. Koike and Y. Nagata (1998b): Bifurcation Current found along the coast of the Kii Peninsula and position of the Kuroshio axis. Acta Oceanographic Taiwanica, 37, 113-125.
Uchida. M., J. Takeuchi, Y. Morikawa, Y. Maekawa. O. Momose, T. Koike and Y. Nagata (2000): On structure and temporal variation of the Bifurcation Current off the Kii Peninsula. J. Oceanogr., 56, 17-30.
