A two-level time-stepping method for layered ocean circulation models: further development and testing
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Publication:556293
DOI10.1016/j.jcp.2004.12.011zbMath1121.86002OpenAlexW1971987074MaRDI QIDQ556293
Publication date: 13 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.2004.12.011
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Related Items (8)
High-order multirate explicit time-stepping schemes for the baroclinic-barotropic split dynamics in primitive equations ⋮ Runge-Kutta IMEX schemes for the Horizontally Explicit/Vertically Implicit (HEVI) solution of wave equations ⋮ Multiple time scales and pressure forcing in discontinuous Galerkin approximations to layered ocean models ⋮ Exponential time differencing for the tracer equations appearing in primitive equation ocean models ⋮ A Second-Order Implicit-Explicit Scheme for the Baroclinic-Barotropic Split System of Primitive Equations ⋮ Pressure forcing and dispersion analysis for discontinuous Galerkin approximations to oceanic fluid flows ⋮ Exponential time differencing for mimetic multilayer Ocean models ⋮ Parallel exponential time differencing methods for geophysical flow simulations
Uses Software
Cites Work
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- Implementation of a barotropic-baroclinic time splitting for isopycnic coordinate ocean modeling
- MPDATA: A finite-difference solver for geophysical flows
- Barotropic-baroclinic time splitting for ocean circulation modeling
- Stable split time stepping schemes for large-scale ocean modeling
- A two-level time-stepping method for layered ocean circulation models
- A synchronous and iterative flux-correction formalism for coupled transport equations
- On the Construction and Comparison of Difference Schemes
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