Pages that link to "Item:Q1418666"

The following pages link to A fully-implicit model of the global ocean circulation (Q1418666):

Displaying 18 items.

• Spin up problem and accelerating convergence to steady state (Q727341) (← links)
• Formulation of an unstructured grid model for global Ocean dynamics (Q1685665) (← links)
• A consistent formulation of the anisotropic stress tensor for use in models of the large-scale ocean circulation (Q1803293) (← links)
• The application of Jacobian-free Newton-Krylov methods to reduce the spin-up time of ocean general circulation models (Q1958932) (← links)
• A communication-avoiding implicit-explicit method for a free-surface ocean model (Q2374967) (← links)
• Corrigendum to ``A tailored solver for bifurcation analysis of ocean-climate models'' (Q2390447) (← links)
• Ocean modelling for climate studies: Eliminating short time scales in long-term, high-resolution studies of ocean circulation (Q2426060) (← links)
• A tailored solver for bifurcation analysis of ocean-climate models (Q2462485) (← links)
• The performance of implicit ocean models on B- and C-grids (Q2572794) (← links)
• (Q3152922) (← links)
• Validation of a Three-Dimensional Model of the Ocean Circulation (Q3650636) (← links)
• (Q4520975) (← links)
• COUPLED BISTABLE MAPS: A TOOL TO STUDY CONVECTION PARAMETERIZATION IN OCEAN MODELS (Q4655614) (← links)
• (Q4877995) (← links)
• Snowball Earth Bifurcations in a Fully-Implicit Earth System Model (Q4990666) (← links)
• The PROSPER General Circulation Model, an adapted form of the Sandia Ocean Modelling method: A numerical description (Q5202453) (← links)
• (Q5705290) (← links)
• A fully implicit model of the three-dimensional thermohaline ocean circulation (Q5956033) (← links)