Transport of Bottom Sediment in the Coastal Sea of Okinawa.
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概要
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Tide-induced residual flow, M<SUB>2</SUB> and M<SUB>4</SUB> tidal currents around Okinawa are caleculated using a horizontal two-dimensional numerical model, and the bottom stress corresponding to that transport is calculated. The estimated direction of bottom sediment trasnport coincides well with the result of field observation in Nakagusuku Bay. The direction of bottom sediment transport around Okinawa is estimated on the basis of calculated results.
- 日本海洋学会の論文
日本海洋学会 | 論文
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