2007
DOI: 10.1016/j.jcp.2006.10.003
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Interactions of breaking waves with a current over cut cells

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Cited by 13 publications
(7 citation statements)
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“…Fig. 2 shows that time history of computed surface elevation at WG2 and WG4 is in good agreement with measurements of Li et al (2007). The small discrepancy at WG4 may be due to the 3-D effect of highly nonlinear waves at WG4 (Li et al, 2007), characterised by a gradual peaking of crests, flattening of troughs and pitching forward to the sea dike.…”
Section: Surface Elevationsupporting
confidence: 63%
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“…Fig. 2 shows that time history of computed surface elevation at WG2 and WG4 is in good agreement with measurements of Li et al (2007). The small discrepancy at WG4 may be due to the 3-D effect of highly nonlinear waves at WG4 (Li et al, 2007), characterised by a gradual peaking of crests, flattening of troughs and pitching forward to the sea dike.…”
Section: Surface Elevationsupporting
confidence: 63%
“…The experiment of wave overtopping over a smooth impermeable dike with a 1:6 seaward slope described by Li et al (2007) was used to validate the RANS-VOF model. Regular waves with a wave height H = 0.16 m and wave period T = 2.0 s was generated by an internal wave-maker, placed at x = −6.1 m with a water depth at the toe of structures of 0.7 m (Fig.…”
Section: Surface Elevationmentioning
confidence: 99%
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“…Multiphase flow is a highly complex multi-scale nonlinear phenomenon, which is encountered in various applications ranging from small-scale droplet interactions [1], microstructural phase evolution in materials [2], flows in oil and natural gas pipelines [3] to large scale free-surface ocean waves and wave breaking [4]. Such kinds of fluid flows can be quite complex to understand and analyze via physical experiments and theoretical ways.…”
Section: Introductionmentioning
confidence: 99%
“…In their model, a wave-maker is established at the inflow boundary by prescribing the inflow velocities, while the current field is gradually introduced in the entire fluid region. Li et al (2007) presented a NS solver using a finite-volume scheme, the volume of fluid (VOF) method and the SGS turbulence model for the interactions between breaking waves and the current over a cut-cell grid. In the case of waves following the current, an external 3 generator combining the inflow motions of the waves and the current is applied at the inflow boundary.…”
Section: Introductionmentioning
confidence: 99%