Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

Shusaku Sugimoto; Kimio Hanawa

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Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

机译：日本南部的黑潮路线与东部的黑潮延伸路线之间的关系

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A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500?m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000?m), the KE path tends to be convoluted, i.e., an unstable state.

机译：使用1993-2008年卫星衍生的测高数据集，研究了黑潮和黑潮扩展（KE）路径之间的关系。当黑潮采取近岸非大曲折路径或典型的大曲折路径并经过伊豆小gas原岭的较深河道（约2500？m）时，KE路径采用相对稳定的状态，并具有两个准平稳曲折。另一方面，当黑潮采取离岸非大曲折路径，然后越过山脊的较浅部分（约1000？m）时，KE路径趋于盘旋，即处于不稳定状态。

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《Journal of oceanography》 |2012年第1期|共7页
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Shusaku Sugimoto; Kimio Hanawa;
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Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

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