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- W4240411166 abstract "When the surface waves propagate in shallow water region, the bottom boundary layer may be turbulent because of sand ripples or other kind of roughness of sea bed. But before the flow becomes fully developed turbulence, there is a state, in a certain range of the Reynolds number, in which the flow is still laminar but has separation and complex structure of vortex. This is termed as quasi-turburent flow in the present paper. The flow structure of this boundary layer affects the mass transport and sedimataion." @default.
- W4240411166 created "2022-05-12" @default.
- W4240411166 creator A5038342653 @default.
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- W4240411166 date "1993-06-24" @default.
- W4240411166 modified "2023-09-25" @default.
- W4240411166 title "Quasi-Turbulent Boundary Layer of Oscillating Flow Over Ripples" @default.
- W4240411166 doi "https://doi.org/10.1061/9780872629332.185" @default.
- W4240411166 hasPublicationYear "1993" @default.
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