A numerical method for the study of the circulation of the world ocean

DOI10.1006/jcph.1997.5699zbMath0938.76070OpenAlexW2150247853MaRDI QIDQ1379886

Kirk Bryan

Publication date: 21 June 2000

Published in: Journal of Computational Physics (Search for Journal in Brave)

Full work available at URL: https://semanticscholar.org/paper/5d3dde8c238dad83753f6c9acc9686028d024aad

zbMATH Keywords

buoyancy forcesbottom topographyequatorial undercurrentrigid-lid approximationfictitious energy generationlarge-scale current systemssurface gravity-inertial waves

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Finite difference methods applied to problems in fluid mechanics (76M20)

Related Items (3)

High-order multirate explicit time-stepping schemes for the baroclinic-barotropic split dynamics in primitive equations ⋮ A Second-Order Implicit-Explicit Scheme for the Baroclinic-Barotropic Split System of Primitive Equations ⋮ Small-time solvability of primitive equations for the ocean with spatially-varying vertical mixing

Cites Work

• Computational design for long-term numerical integration of the equations of fluid motion: two-dimensional incompressible flow. Part I
• A global numerical ocean model. I
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