4.7 Article

Assessment of Numerical Methods for Plunging Breaking Wave Predictions

Journal

Publisher

MDPI
DOI: 10.3390/jmse9030264

Keywords

air-water interface modeling; plunging wave breaking; volume-of-fluid method

Funding

  1. Engineering Research & Development Center [W912HZ-17-2-0014]

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This study evaluates the capability of Navier-Stokes solvers in predicting plunging breaking, showing that different parameters have an impact on predictions, and suggesting the selection of appropriate grid resolution and models for different test cases; experiments indicate that finer grids can accurately predict splash-up events but may induce interface instabilities.
This study evaluates the capability of Navier-Stokes solvers in predicting forward and backward plunging breaking, including assessment of the effect of grid resolution, turbulence model, and VoF, CLSVoF interface models on predictions. For this purpose, 2D simulations are performed for four test cases: dam break, solitary wave run up on a slope, flow over a submerged bump, and solitary wave over a submerged rectangular obstacle. Plunging wave breaking involves high wave crest, plunger formation, and splash up, followed by second plunger, and chaotic water motions. Coarser grids reasonably predict the wave breaking features, but finer grids are required for accurate prediction of the splash up events. However, instabilities are triggered at the air-water interface (primarily for the air flow) on very fine grids, which induces surface peel-off or kinks and roll-up of the plunger tips. Reynolds averaged Navier-Stokes (RANS) turbulence models result in high eddy-viscosity in the air-water region which decays the fluid momentum and adversely affects the predictions. Both VoF and CLSVoF methods predict the large-scale plunging breaking characteristics well; however, they vary in the prediction of the finer details. The CLSVoF solver predicts the splash-up event and secondary plunger better than the VoF solver; however, the latter predicts the plunger shape better than the former for the solitary wave run-up on a slope case.

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