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- W2330891081 abstract "The net current (streaming) in the bottom boundary layer under waves is mainly determined by two competing mechanisms, namely an offshore streaming related to the non-linearity of the wave shape and an onshore streaming resulting from the horizontal non-uniformity of the velocity field under free surface waves. This paper describes a Reynolds-averaged boundary layer model with k-e turbulence closure that includes both streaming processes. The model is validated on measurements and applied for a numerical study on the balance between the two streaming mechanisms. The results show an increasing importance of the offshore streaming over the onshore streaming for decreasing relative water depth and for decreasing relative bed roughness. Qualitatively, the effect of changing water depth on streaming agrees well with analytical results from literature. We therefore consider the model as a trustworthy framework for future research on the role of wave-induced streaming on sediment transport." @default.
- W2330891081 created "2016-06-24" @default.
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- W2330891081 date "2011-04-01" @default.
- W2330891081 modified "2023-09-25" @default.
- W2330891081 title "NET CURRENTS IN THE WAVE BOUNDARY LAYER: BALANCE OF WAVE SHAPE AND FREE SURFACE EFFECTS" @default.
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- W2330891081 doi "https://doi.org/10.1142/9789814355537_0113" @default.
- W2330891081 hasPublicationYear "2011" @default.
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