Pages that link to "Item:Q1013179"
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The following pages link to On the time-splitting scheme used in the Princeton ocean model (Q1013179):
Displaying 9 items.
- A two-level time-stepping method for layered ocean circulation models: further development and testing (Q556293) (← links)
- A comparison of time discretization schemes for two-timescale problems in geophysical fluid dynamics (Q697714) (← links)
- Implementation of a barotropic-baroclinic time splitting for isopycnic coordinate ocean modeling (Q1282434) (← links)
- Stable split time stepping schemes for large-scale ocean modeling (Q1368627) (← links)
- A two-level time-stepping method for layered ocean circulation models (Q1604447) (← links)
- High-order multirate explicit time-stepping schemes for the baroclinic-barotropic split dynamics in primitive equations (Q2135813) (← links)
- Comparison of exponential integrators and traditional time integration schemes for the shallow water equations (Q2154874) (← links)
- Stability analysis of split-explicit free surface ocean models: implication of the depth-independent barotropic mode approximation (Q2222560) (← links)
- The influence of time step size on the results of numerical modeling of global ocean climate (Q5407684) (← links)