Uniformly high-order accurate nonoscillatory schemes
SIAM Journal on Numerical Analysis
Efficient implementation of essentially non-oscillatory shock-capturing schemes
Journal of Computational Physics
Non-oscillatory central differencing for hyperbolic conservation laws
Journal of Computational Physics
Weighted essentially non-oscillatory schemes
Journal of Computational Physics
Journal of Computational Physics
Numerical modelling of two-way propagation of non-linear dispersive waves
Mathematics and Computers in Simulation - IMACS sponsored special issue on nonlinear waves: computation and theory
A Local Discontinuous Galerkin Method for KdV Type Equations
SIAM Journal on Numerical Analysis
A New Class of Optimal High-Order Strong-Stability-Preserving Time Discretization Methods
SIAM Journal on Numerical Analysis
Local discontinuous Galerkin methods for nonlinear dispersive equations
Journal of Computational Physics
A Fast and Stable Well-Balanced Scheme with Hydrostatic Reconstruction for Shallow Water Flows
SIAM Journal on Scientific Computing
Spectral/hp discontinuous Galerkin methods for modelling 2D Boussinesq equations
Journal of Computational Physics
Numerical solution of KdV-KdV systems of Boussinesq equations
Mathematics and Computers in Simulation
Mathematics and Computers in Simulation
Numerical solution of Boussinesq systems of the Bona--Smith family
Applied Numerical Mathematics
High order well-balanced CDG-FE methods for shallow water waves by a Green-Naghdi model
Journal of Computational Physics
Hi-index | 31.46 |
Finite volume schemes are commonly used to construct approximate solutions to conservation laws. In this study we extend the framework of the finite volume methods to dispersive water wave models, in particular to Boussinesq type systems. We focus mainly on the application of the method to bidirectional nonlinear, dispersive wave propagation in one space dimension. Special emphasis is given to important nonlinear phenomena such as solitary waves interactions, dispersive shock wave formation and the runup of breaking and non-breaking long waves.