2000
DOI: 10.1006/jcph.2000.6426
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Large-Wave Simulation (LWS) of Free-Surface Flows Developing Weak Spilling Breaking Waves

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Cited by 26 publications
(30 citation statements)
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“…A boundary-fitted transformation is introduced to obtain a time-independent computational domain and facilitate filtering of the flow equations according to the LWS formulation (Dimas and Fialkowski, 2000). The transformed coordinates are…”
Section: Lws Formulationmentioning
confidence: 99%
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“…A boundary-fitted transformation is introduced to obtain a time-independent computational domain and facilitate filtering of the flow equations according to the LWS formulation (Dimas and Fialkowski, 2000). The transformed coordinates are…”
Section: Lws Formulationmentioning
confidence: 99%
“…The model is based on the large-wave simulation (LWS) formulation, which was originally developed for two-dimensional, deep-water breaking (Dimas and Fialkowski, 2000) and is adapted here for application to three-dimensional, coastal breaking. LWS is based on the decomposition of flow scales, related to velocity, pressure and free-surface elevation, into resolved (large) and subgrid (small) scales.…”
Section: Introductionmentioning
confidence: 99%
“…The interaction between a gravity wave and a drift layer of non-zero thickness (see sketch in Fig. 1) was considered in [9,10] utilizing experimental measurements and numerical simulations. In the laboratory, the drift layer was induced by towing a plastic sheet on the water surface ahead of the gravity wave, which was generated by towing a two-dimensional fully-submerged hydrofoil in the same direction and at the same constant speed C as the sheet.…”
Section: Introductionmentioning
confidence: 99%
“…(1). The new incipient breaking criterion was also established numerically in [10] utilizing the large-wave simulation (LWS) methodology. The model, though, considered in [9,10], corresponds to a wavelength of about 0.5 m, while the wavelengths measured in [3,4] are smaller.…”
Section: Introductionmentioning
confidence: 99%
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