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Improving the Performances of a Novel RANS Model for Breaking Water Waves Using a Subgrid Approach and Non-equidistant Layers

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Abstract

Numerical models used in coastal engineering must be computationally efficient while maintaining accuracy at an engineering level. One major weakness of models based on non-hydrostatic Reynolds Averaged Navier–Stokes (RANS) equations is the solution of the Poisson equation used to evolve pressure values over time, accounting for up to 70% of the computational time. We propose a method that uses a differential grid to reduce the computational costs while maintaining a good accuracy: a “subgrid approach”, in which pressure values are computed on a coarse grid while velocities are solved on a finer grid. In addition, the grid resolution is increased near the surface and bottom boundaries. This approach is applied to Iravani et al. (Coast Eng 159:103717, 2020. https://doi.org/10.1016/j.coastaleng.2020.103717) model, which also implements novel free surface boundary conditions for breaking waves. The results show how the computational effort can be reduced up to 70% while providing more than satisfactory results for properties of interest for the coastal engineering practice, like wave height decay and mean water elevation.

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The datasets generated during and analyzed during the current study are available from the corresponding author on reasonable request.

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Correspondence to Nikta Iravani.

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Appendix

Appendix

The following figures show the comparison between numerical results and experimental data of Ting and Kirby [8] for the TKE and velocity profiles. As indicated in the captions, different grid configurations and numerical methods are used Figs. 16, 17, 18, 19, 20, 21, 22.

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Vertical profiles of the averaged TKE and averaged horizontal velocities at different measuring stations with different numbers of non-equidistant layers (two upper layers and two lower layers have a thickness equal to 0.05)

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Vertical profiles of averaged TKE and averaged horizontal velocities at different measuring stations for a 10-layer grid with different numbers of fine layers near the surface and the bottom

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Vertical profiles of averaged horizontal velocity and averaged TKE using different numbers of layers for the coarse grid

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Comparison between the numerical results and the experimental data of the Spilling breaker case of Ting & Kirby for the time-averaged velocities and time-averaged TKE. a Solving the momentum equation on the fine grid (blue dotted line), b solving the vertical momentum equation on the coarse grid (continuous red line)

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Comparison between the numerical results and the experimental data of the Spilling breaker case of Ting & Kirby. Different resolutions have been used for the fine and coarse grid

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Comparison between the numerical results and the experimental data of the Spilling breaker case of Ting and Kirby. a Solving the vertical momentum equation on the coarse grid (green dotted line), b solving the vertical momentum equation on the fine grid (continuous red line)

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Comparison between the numerical results and the experimental data of the Spilling breaker case of Ting & Kirby. a Linear pressure interpolation (blue dotted line), b Spline interpolation (continuous red line)

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Iravani, N., Badiei, P. & Brocchini, M. Improving the Performances of a Novel RANS Model for Breaking Water Waves Using a Subgrid Approach and Non-equidistant Layers. Water Waves 4, 447–490 (2022). https://doi.org/10.1007/s42286-022-00066-4

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