Abstract

Two methods for computing local mass flux for a continuous Galerkin finite element formulation of the Generalized Wave Continuity Equation (GWCE) are derived and a third method is discussed in light of the first two. The GWCE is shown to not conserve mass locally, while it can be shown to conserve a certain quantity locally. The two derived methods are demonstrated for a realistic tidal flow problem in the Bight of Abaco, Bahamas.

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