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A Conforming Finite Element Discretization of the Streamfunction Form of the Unsteady Quasi-Geostrophic Equations

This paper presents a conforming finite element semi-discretization of the streamfunction form of the one-layer unsteady quasi-geostrophic equations, which are a commonly used model for large-scale wind-driven ocean circulation. We derive optimal error estimates and present numerical results.

preprint2014arXivOpen access
Erich L FosterTraian IliescuDavid R. Wells
math.NA
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Erich L FosterTraian IliescuDavid R. Wells

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