Jing Yuan 1 , Dongxu Wang 1 Plain Language Summary In shallow coastal regions, shoaling waves produce oscillatory bottom flows, which create sand 3 ripples on a sandy seabed. The acceleration skewness of the oscillatory flow is a result of the 4 nonlinear feature of the overlying water waves, and it can differentiate the two half-cycles of 5 the oscillatory flow and therefore leading to a net (cycle-averaged) sediment transport. In this 6 study, we use an oscillatory water tunnel and particle image velocimetry to investigate the oscil7 latory boundary layer flow over vortex ripples with a focus on the effect of acceleration skewness. 8 Our measurements provide detailed descriptions of the formation-ejection process of coherent 9 vortices, which is produced by the flow separation behind the ripple crest. Some useful observa10 tions on flow turbulence are also provided. The results showed that acceleration skewness can 11 substantially differentiate the two coherent vortices developed within the two half cycles. The 12 offshore-side vortex can carry more turbulence over the ripple crest than the onshore-side vortex, 13 which possibly leads to some net onshore sediment transport rate. We also showed that the 14 ripple-averaged flow is fairly close to that over a flat bed, so flat-bed boundary layer model can 15 be possibly used for rippled bed with some parameterizations. 16
An Experimental Investigation of Acceleration‐Skewed Oscillatory Flow Over Vortex Ripples
Published 2019 in Journal of Geophysical Research
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PUBLICATION RECORD
- Publication year
2019
- Venue
Journal of Geophysical Research
- Publication date
2019-12-01
- Fields of study
Geology, Environmental Science
- Identifiers
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