2015
DOI: 10.1016/j.oceaneng.2015.08.030
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Generation of free-surface waves by localized source terms in the continuity equation

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Cited by 26 publications
(23 citation statements)
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“…For many scientific or industrial applications, wavemakers with sophisticated theoretical solutions are used, although transient time traces require calibration, practically making the details of the wavemaker transfer function irrelevant and even creating an unnecessary overhead [23]. Applying a calibrated two-dimensional result to a corresponding three-dimensional domain is efficient and is also the recommended approach by Perić and Abdel-Maksoud [24].…”
Section: Impulse Source Wavemakermentioning
confidence: 99%
“…For many scientific or industrial applications, wavemakers with sophisticated theoretical solutions are used, although transient time traces require calibration, practically making the details of the wavemaker transfer function irrelevant and even creating an unnecessary overhead [23]. Applying a calibrated two-dimensional result to a corresponding three-dimensional domain is efficient and is also the recommended approach by Perić and Abdel-Maksoud [24].…”
Section: Impulse Source Wavemakermentioning
confidence: 99%
“…A third method is to embed the wavemaker within the model domain with the addition of sponge layers for wave damping at the boundaries (e.g., Larsen and Dancy, 1983;Wei et al, 1999;Lin and Liu, 1999;Lara et al, 2006). The method has been used in both Boussinesqtype (e.g., Wei et al, 1999;Schäffer and Sørensen, 2006;Kim et al, 2007;Liam et al, 2014) and RANS models (e.g., Lin and Liu, 1999;Hafsia et al, 2009;Perić and Abdel-Maksoud, 2015) and avoids the complication of both generating and absorbing waves at a boundary. Internal wavemakers first generated waves on a single line (cross-shore delta function) source (Larsen and Dancy, 1983), which continues to be used in Boussinesq models (e.g., Schäffer and Sørensen, 2006;Kim et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…For wave generation, five different methods are well known: the Relaxation Zone Method (RZM) [34,40,41], Static (SBM) and Dynamic Boundary Method (DBM) [9,42], Mass Source Method (MSM) [43,44] and Impulse Source Method (ISM) [45][46][47][48]. For numerical wave absorption, six different methods are available, i.e., the RZM, SBM, DBM, Numerical Beach (NB) implementations [2,49], geometrically sloped beaches [50][51][52] and the cell stretching method [53].…”
Section: Methodsmentioning
confidence: 99%