Multilevel schemes for the shallow water equations
From MaRDI portal
Publication:1781594
DOI10.1016/j.jcp.2005.01.025zbMath1213.76132OpenAlexW2053112652MaRDI QIDQ1781594
F. Jauberteau, Joseph J. Tribbia, Thierry Dubois, Roger M. Temam
Publication date: 27 June 2005
Published in: Journal of Computational Physics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.jcp.2005.01.025
Lua error in Module:PublicationMSCList at line 37: attempt to index local 'msc_result' (a nil value).
Related Items (5)
Multilevel finite volume methods and boundary conditions for geophysical flows ⋮ Multiscale/fractional step schemes for the numerical simulation of the rotating shallow water flows with complex periodic topography ⋮ A two-grid finite difference method for the primitive equations of the ocean ⋮ A time-filtering method for plasma simulation: high bulk conductivity ⋮ A Monge-Ampère enhancement for semi-Lagrangian methods
Cites Work
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- A comparison of time discretization schemes for two-timescale problems in geophysical fluid dynamics
- Incremental unknowns for solving partial differential equations
- Two-layer shallow-water flow in two dimensions, a numerical study
- Nonlinear Galerkin method and subgrid-scale model for two-dimensional turbulent flows
- A dynamic multilevel model for the simulation of the small structures in homogeneous isotropic turbulence
- On simulating flows with multiple time scales using a method of averages
- Time explicit schemes and spatial finite differences splittings
- Incremental unknowns, multilevel methods and the numerical simulation of turbulence
- On balanced approximations for time integration of multiple time scale systems.
- Numerical Methods Based on Additive Splittings for Hyperbolic Partial Differential Equations
- Comparison of Numerical Methods for the Calculation of Two-Dimensional Turbulence
- Theoretical and Practical Aspects of Some Initial Boundary Value Problems in Fluid Dynamics
- Incremental unknowns on nonuniform meshes
- The stress generated in a non-dilute suspension of elongated particles by pure straining motion
This page was built for publication: Multilevel schemes for the shallow water equations