2020
DOI: 10.1016/j.coastaleng.2019.103583
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An experimental study of net sediment transport rate due to acceleration-skewed oscillatory flows over rippled seabeds

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Cited by 6 publications
(28 citation statements)
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“…(2007), Frank-Gilchrist et al. (2018) and Wang & Yuan (2020), show that this intensified shear stress erodes sediment in the stoss side and creates a strong sediment flux toward the ripple crest and the lee side of the ripple. The thick lines in figure 16( b ) are the corresponding turbulence-averaged streamwise components of the shear stress on the ripple shown in figure 14( b ).…”
Section: Ripple Dimensions and Fluid Kinematicsmentioning
confidence: 97%
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“…(2007), Frank-Gilchrist et al. (2018) and Wang & Yuan (2020), show that this intensified shear stress erodes sediment in the stoss side and creates a strong sediment flux toward the ripple crest and the lee side of the ripple. The thick lines in figure 16( b ) are the corresponding turbulence-averaged streamwise components of the shear stress on the ripple shown in figure 14( b ).…”
Section: Ripple Dimensions and Fluid Kinematicsmentioning
confidence: 97%
“…These sediment-laden vortices are eventually washed over the ripple crests and ejected into the water column at the opposite side of the ripple during the flow reversal. Meanwhile, sediment trapped within these vortices deposits back to the opposite side of the ripple surface, repairing the erosion that occurred on the previous half-cycle (van der Werf et al 2007;Ribberink et al 2008;Wang & Yuan 2020). The prominent vortex kinematics and the associated sediment transport processes respond rapidly to the disequilibrium in the above coordination, which eventually leads to changes in the ripple morphology.…”
Section: Introductionmentioning
confidence: 94%
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