The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves

Ocean wave breaking is a difficult-to-model oceanographic process, which has implications for extreme wave statistics, the dissipation of wave energy, and air-sea interaction. Numerical methods capable of reliably simulating real-world directionally spread breaking waves are useful for investigating...

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Main Authors: Kanehira, T, McAllister, ML, Draycott, S, Nakashima, T, Ingram, DM, van den Bremer, TS, Mutsuda, H
Format: Journal article
Language:English
Published: Springer 2022
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author Kanehira, T
McAllister, ML
Draycott, S
Nakashima, T
Ingram, DM
van den Bremer, TS
Mutsuda, H
author_facet Kanehira, T
McAllister, ML
Draycott, S
Nakashima, T
Ingram, DM
van den Bremer, TS
Mutsuda, H
author_sort Kanehira, T
collection OXFORD
description Ocean wave breaking is a difficult-to-model oceanographic process, which has implications for extreme wave statistics, the dissipation of wave energy, and air-sea interaction. Numerical methods capable of reliably simulating real-world directionally spread breaking waves are useful for investigating the physics of wave breaking and for the design of offshore structures and floating bodies. Smoothed Particle Hydrodynamics (SPH) is capable of modelling highly steep and overturning free surfaces, which makes it a promising method for simulating breaking waves. This paper investigates the effect of smoothing length on simulated wave breaking in both following and crossing seas. To do so, we reproduce numerically the experiments of highly directionally spread breaking waves in McAllister et al. [J. Fluid Mech. vol. 860, 2019, pp. 767–786] using a range of normalised smoothing lengths: h/dp =1.4, 1.7, 2.0, 2.3, with h smoothing length and dp particle spacing. The smallest smoothing length we use appears to adversely affect the fidelity of the simulated surface elevation, so that the tallest wave crest observed in experiments is not fully reproduced (coefficient of determination r 2 ≈ 0.7). For smoothing lengths h/dp = 1.7, 2.0, and 2.3, the experiments are well reproduced (r 2 ≥ 0.88); in these simulations smoothing length predominantly affects the spatial extent and duration of breaking. Qualitative and quantitative comparison of our simulations show that values of h/dp in the range 1.7 − 2 best reproduce the wave breaking phenomena observed in experiments.
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spelling oxford-uuid:f9b84326-9855-4a8a-b2de-e0ea27faa0572023-02-07T08:30:19ZThe effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread wavesJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:f9b84326-9855-4a8a-b2de-e0ea27faa057EnglishSymplectic ElementsSpringer2022Kanehira, TMcAllister, MLDraycott, SNakashima, TIngram, DMvan den Bremer, TSMutsuda, HOcean wave breaking is a difficult-to-model oceanographic process, which has implications for extreme wave statistics, the dissipation of wave energy, and air-sea interaction. Numerical methods capable of reliably simulating real-world directionally spread breaking waves are useful for investigating the physics of wave breaking and for the design of offshore structures and floating bodies. Smoothed Particle Hydrodynamics (SPH) is capable of modelling highly steep and overturning free surfaces, which makes it a promising method for simulating breaking waves. This paper investigates the effect of smoothing length on simulated wave breaking in both following and crossing seas. To do so, we reproduce numerically the experiments of highly directionally spread breaking waves in McAllister et al. [J. Fluid Mech. vol. 860, 2019, pp. 767–786] using a range of normalised smoothing lengths: h/dp =1.4, 1.7, 2.0, 2.3, with h smoothing length and dp particle spacing. The smallest smoothing length we use appears to adversely affect the fidelity of the simulated surface elevation, so that the tallest wave crest observed in experiments is not fully reproduced (coefficient of determination r 2 ≈ 0.7). For smoothing lengths h/dp = 1.7, 2.0, and 2.3, the experiments are well reproduced (r 2 ≥ 0.88); in these simulations smoothing length predominantly affects the spatial extent and duration of breaking. Qualitative and quantitative comparison of our simulations show that values of h/dp in the range 1.7 − 2 best reproduce the wave breaking phenomena observed in experiments.
spellingShingle Kanehira, T
McAllister, ML
Draycott, S
Nakashima, T
Ingram, DM
van den Bremer, TS
Mutsuda, H
The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title_full The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title_fullStr The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title_full_unstemmed The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title_short The effects of smoothing length on the onset of wave breaking in Smoothed Particle Hydrodynamics (SPH) simulations of highly directionally spread waves
title_sort effects of smoothing length on the onset of wave breaking in smoothed particle hydrodynamics sph simulations of highly directionally spread waves
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