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- W2324973726 abstract "Fundamental features of transitional distributions of velocity and shear in a run-up wave have been experimentally identified in this paper. In the run-up front, vertically uniform shore-ward velocity is predominant, while typical free-surface shearing flow with a bottom boundary layer is formed behind the front. Depending on local surface gradients and fluid acceleration, reverse streaming occurs within the boundary layer despite the shore-ward flow still dominates above the layer. In the later stage, another shear layer has also been formed beneath the surface." @default.
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- W2324973726 date "2012-01-01" @default.
- W2324973726 modified "2023-09-27" @default.
- W2324973726 title "Transitional velocity and shear distributions in a runup wave" @default.
- W2324973726 cites W2162994978 @default.
- W2324973726 doi "https://doi.org/10.2208/kaigan.68.i_56" @default.
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