2018
DOI: 10.1016/j.apm.2017.12.005
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An improved Serre model: Efficient simulation and comparative evaluation

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Cited by 11 publications
(4 citation statements)
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“…Note that a time shift of 0.2 s was needed to match the results at the first station, and this time shift is therefore applied at all stations. As noted in do Carmo et al (2018), this lag is may be explained by the physical difference between the initial condition used in the simulations and the removal of the dam in the experiment of do Carmo et al (1993). All computations agree well with the experiments at the first station ( Figure 5(b)) but overestimate the height of the front wave at the next two stations ( Figures 5(c) and (d)).…”
Section: Dam-break Experiments Of Dosupporting
confidence: 62%
“…Note that a time shift of 0.2 s was needed to match the results at the first station, and this time shift is therefore applied at all stations. As noted in do Carmo et al (2018), this lag is may be explained by the physical difference between the initial condition used in the simulations and the removal of the dam in the experiment of do Carmo et al (1993). All computations agree well with the experiments at the first station ( Figure 5(b)) but overestimate the height of the front wave at the next two stations ( Figures 5(c) and (d)).…”
Section: Dam-break Experiments Of Dosupporting
confidence: 62%
“…Taking advantage of a solving methodology, which encompasses the Serre and Saint-Venant systems of equations, the wave-breaking strategy detailed in [26] is used, which consists of switching locally from the system of Serre equations to the Saint-Venant equations when the wave is about to break. Breaking is easily incorporated simply by ignoring the contribution of the dispersive terms included in the parameter σ 2 of Equation (3) (see [26] for details).…”
Section: Wave Breaking Strategymentioning
confidence: 99%
“…It is also worth pointing out that for the simulation of more complex problems, such as wave generation by seafloor movement [15], the propagation of waves over uneven bottoms [16,17], the propagation of high-frequency waves resulting from nonlinear interactions and wave-breaking effects [18][19][20], extended forms of Boussinesq and Serre equations have been developed in recent years with improved linear characteristics [21][22][23][24][25][26].…”
Section: Introductionmentioning
confidence: 99%
“…For wave generation, FLOW-3D® has the ability to simulate surface waves of regular linear and non-linear propagation, as well as irregular waves. Although linear wave theory [30] has been used in many applications, non-linear wave theories generally offer a significant improvement in accuracy over linear wave theory for greater wave amplitudes [31]. In FLOW-3D®, three theories of non-linear waves are used to generate non-linear waves: (a) Stokes 5 th order wave theory [32], (b) Fourier series method for Stokes and cnoidal waves [33] and (c) McCowan's theory for solitary waves [34].…”
Section: Breakwater Geometrymentioning
confidence: 99%