A two-level finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the ocean

DOI10.1016/j.camwa.2013.07.025zbMath1381.86003arXiv1211.0958OpenAlexW2095569981MaRDI QIDQ316202

Traian Iliescu, Erich L. Foster, David R. Wells

Publication date: 26 September 2016

Published in: Computers \& Mathematics with Applications (Search for Journal in Brave)

Full work available at URL: https://arxiv.org/abs/1211.0958

zbMATH Keywords

finite element methodArgyris elementquasi-geostrophic equationsstreamfunction formulationtwo-level algorithm

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Finite element, Rayleigh-Ritz and Galerkin methods for boundary value problems involving PDEs (65N30) Finite element methods applied to problems in fluid mechanics (76M10) Computational methods for problems pertaining to geophysics (86-08)

Related Items (4)

Numerical study of a regularized barotropic vorticity model of geophysical flow ⋮ Two-level method for the total fractional-order variation model in image deblurring problem ⋮ B-spline based finite-element method for the stationary quasi-geostrophic equations of the Ocean ⋮ Two-level Galerkin Mixed Finite Element Method for Darcy--Forchheimer Model in Porous Media

Uses Software

• Algorithm 884

Cites Work

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