A large time step upwind scheme for the shallow water equations with source terms

2012 ◽  
pp. 141-148 ◽  
Author(s):  
M Morales-Hernandez ◽  
J Murillo ◽  
P García-Navarro ◽  
J Burguete
2017 ◽  
Vol 15 (3) ◽  
pp. 765-788 ◽  
Author(s):  
Christophe Chalons ◽  
Pierre Kestener ◽  
Samuel Kokh ◽  
Maxime Stauffert

2012 ◽  
Vol 231 (19) ◽  
pp. 6532-6557 ◽  
Author(s):  
M. Morales-Hernandez ◽  
P. García-Navarro ◽  
J. Murillo

2014 ◽  
Vol 59 (21) ◽  
pp. 2534-2540 ◽  
Author(s):  
Renyi Xu ◽  
Deyu Zhong ◽  
Baosheng Wu ◽  
Xudong Fu ◽  
Runze Miao

2011 ◽  
Vol 2011 ◽  
pp. 1-17 ◽  
Author(s):  
Montri Maleewong

A modified predictor-corrector scheme combining with the depth gradient method (DGM) and the weighted average flux (WAF) method has been presented to solve the one-dimensional shallow water equations with source terms. Approximate solutions in the predictor step are obtained by the DGM with piecewise-linear reconstructions in each cell volume. The source terms can then be calculated directly by these predicted values at the corresponding half-time step. In the corrector step, the TVD version of the WAF method is applied to calculate the numerical fluxes at the same half-time step for each cell face. The accuracy of numerical solutions is shown by applying the method to solve various test cases in both steady and unsteady problems with and without source terms. It shows that the numerical results are in good agreement with the existing analytical solutions as well as experimental data in some test cases.


2014 ◽  
Vol 16 (2) ◽  
pp. 307-347 ◽  
Author(s):  
Georgij Bispen ◽  
K. R. Arun ◽  
Mária Lukáčová-Medvid’ová ◽  
Sebastian Noelle

AbstractWe present new large time step methods for the shallow water flows in the low Froude number limit. In order to take into account multiscale phenomena that typically appear in geophysical flows nonlinear fluxes are split into a linear part governing the gravitational waves and the nonlinear advection. We propose to approximate fast linear waves implicitly in time and in space by means of a genuinely multidimensional evolution operator. On the other hand, we approximate nonlinear advection part explicitly in time and in space by means of the method of characteristics or some standard numerical flux function. Time integration is realized by the implicit-explicit (IMEX) method. We apply the IMEX Euler scheme, two step Runge Kutta Cranck Nicolson scheme, as well as the semi-implicit BDF scheme and prove their asymptotic preserving property in the low Froude number limit. Numerical experiments demonstrate stability, accuracy and robustness of these new large time step finite volume schemes with respect to small Froude number.


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