A new Boussinesq method for fully nonlinear waves from shallow to deep water
By P. A. Madsen, Harry B. Bingham, Hua Liu. Journal of Fluid Mechanics, 2002
366 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ocean Engineering, Oceanography
View Paper: https://www.semanticscholar.org/paper/d7a50cb6f3ad1ab8e9b58898e36c685e3414a421
How researchers see this paper
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In Earth-Surface Processes
- P. A. Madsen
- D. Fuhrman
- H. Schäffer
- Benlong Wang
- Harry B. Bingham
- David Lannes
- Philippe Bonneton
- Stéphane Popinet
In Ocean Engineering
In Oceanography
- P. A. Madsen
- H. Schäffer
- D. Fuhrman
- Philippe Bonneton
- Benlong Wang
- Harry B. Bingham
- David Lannes
- Stéphane Popinet
Citations in the corpus
- A Boussinesq-type method for fully nonlinear waves interacting with a rapidly varying bathymetry (2006, methodology): “…0.5h, in which case the vertical distribu- tion of the velocity field in fully nonlinear waves is accurate for wave numbers in the interval 0 kh 12 while the dispersion relation and non-linear wave–wave interaction properties are accurate in the interval of 0 kh 25 (see Madsen et al., 2002, 2003).”
- Boussinesq-type formulations for fully nonlinear and extremely dispersive water waves: derivation and analysis (2003, methodology): “A more complete description of the numerical implementation, along with a number of illustrative calculations, can be found in Madsen et al. (2002). The solution is obtained over a grid of N equally spaced points and at equally spaced time-steps (only one horizontal dimension is discussed here).”
- A two-layer approach to wave modelling (2004, neutral): “Madsen et al .”
- A new level set numerical wave tank with improved density interpolation for complex wave hydrodynamics (2016, background): “Extended versions of the Boussinesq equations make it possible to predict wave propagation and transformation from deep to shallow water with the help of improved dispersive terms [29].”
- Derivation of asymptotic two-dimensional time-dependent equations for surface water wave propagation (2009, background): “This is the case because the expansion (29) keeps the nonlocal eects of the Dirichlet-Neumann operator Gµ[",b ] . In [41, 42, 43 ], the authors make a dierential approximation of shallow water type based on Pad´e approximants; they show that the dispersive properties remain good far beyond the shal”
- On the solitary wave paradigm for tsunamis (2008, methodology): “A detailed description of the scheme can be found in Madsen et al. [2002] for one horizontal dimension, and in Fuhrman and Bingham [2004] for two horizontal dimensions.”