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- W3146881331 abstract "The residual currents in Tokyo Bay during four seasons are calculated diagnostically from the observed water temperature, salinity and wind data collected by Unoki et al. (1980). The calculated residual currents, verified by the observed ones, show an obvious seasonal variable character. During spring, a clear anticlockwise circulation develops in the head region of the bay and a strong southwestward current flows in the upper layer along the eastern coast f rom the central par t to the mouth ofthe bay. During summer, the anticlockwise circulation in the head region is maintained but the southwestward current along the eastern coast becomes weak. During autumn, the preceding anticlockwise circulation disappears but a clockwise circulation develops in the central par t of the bay. During winter, the calculated residual current is similar to that during autumn. As a conclusion, the seasonal variation of residual current in Tokyo Bay can be at tr ibuted to the variation of the strength of two eddies. The first one is the anticlockwise circulation in the head region ofthe bay, which develops in spring and summer and disappears in autumn and winter. The second one is the clockwise circulation in the central part of the bay, which develops in autumn and winter, decreases in spring and nearly disappears in summer." @default.
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- W3146881331 date "2005-01-01" @default.
- W3146881331 modified "2023-09-26" @default.
- W3146881331 title "Seasonal Variation of ResiduAl Current in Tokyo Bay, Japan Diagnostic Numerical Experiments" @default.
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