2008
DOI: 10.1002/fld.1846
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A high‐order Petrov–Galerkin finite element method for the classical Boussinesq wave model

Abstract: SUMMARYA high-order Petrov-Galerkin finite element scheme is presented to solve the one-dimensional depthintegrated classical Boussinesq equations for weakly non-linear and weakly dispersive waves. Finite elements are used both in the space and the time domains. The shape functions are bilinear in spacetime, whereas the weighting functions are linear in space and quadratic in time, with C 0 -continuity. Dispersion correction and a highly selective dissipation mechanism are introduced through additional streaml… Show more

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Cited by 13 publications
(7 citation statements)
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“…Finite difference (FD) schemes [39,43,47], finite element methods [7,15,28,58] and spectral methods [60,62] have been proposed. More contemporary discontinuous Galerkin (DG) schemes have also been adapted with some success to dispersive wave equations [33,34,53,79] while the application of Finite Volumes (FV) or hybrid FV/FD methods remain most infrequent for this type of problems.…”
Section: Introductionmentioning
confidence: 99%
“…Finite difference (FD) schemes [39,43,47], finite element methods [7,15,28,58] and spectral methods [60,62] have been proposed. More contemporary discontinuous Galerkin (DG) schemes have also been adapted with some success to dispersive wave equations [33,34,53,79] while the application of Finite Volumes (FV) or hybrid FV/FD methods remain most infrequent for this type of problems.…”
Section: Introductionmentioning
confidence: 99%
“…And knowledge about the hydrodynamic patterns influenced by bottom morphological changes may allow assessment and forecasting of the effects of hazardous and extreme events, anthropogenic intervention, or climate change. Hydrodynamic modeling has therefore been the focus of a large number of previous works in estuarine environments [11,14,17,21,22,[40][41][42][43][44][45][46][47][48][49][50].…”
Section: Numerical Models and The Ensembles Techniquementioning
confidence: 99%
“…3) 4) with φ being the velocity potential (by definition, the irrotational velocity field (u, v) = (∇φ, ∂ y φ), g the acceleration due to the gravity force and ∇ = (∂ x 1 , ∂ x 2 ) denotes the gradient operator in horizontal Cartesian coordinates and |∇φ| 2 ≡ (∇φ) · (∇φ). The incompressibility condition leads to the Laplace equation for φ.…”
Section: Mathematical Modelmentioning
confidence: 99%