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?

Yoshihiko Sekine; Koh-ichi FUJITA

doi:10.1023/a:1007857005988

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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?

Yoshihiko Sekine, Koh-ichi FUJITA

Journal of Oceanography1999doi:10.1023/a:1007857005988

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Abstract

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Authors

Yoshihiko Sekine#1 Koh-ichi FUJITA#2

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Mie University

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On Structure and Temporal Variation of the Bifurcation Current off the Kii Peninsula

2000 · 6 citations

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10.1007/bf02276747

10.1007/bf02276747 · 1993

10.1007/bf02312095

10.1007/bf02312095 · 1980

10.1007/bf02109238

10.1007/bf02109238 · 1985

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?

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