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A mixed discontinuous/continuous finite element pair for shallow-water ocean modelling

机译:浅水海洋建模的混合不连续/连续有限元对

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We introduce a mixed discontinuous/continuous finite element pair for ocean modelling, with continuous quadratic layer thickness and discontinuous velocity. We investigate the finite element pair applied to the linear shallow-water equations on an f-plane. The element pair has the property that all geostrophically balanced states which strongly satisfy the boundary conditions have discrete divergence equal to exactly zero and hence are exactly steady states of the discretised equations. This means that the finite element pair has excellent geostrophic balance properties. We also show that the element pair applied to the non-rotating linear shallow-water equations does not have any spurious small eigenvalues. We illustrate these properties using numerical tests and provide convergence calculations which show that the numerical solutions have errors which decay quadratically with element edge length for both velocity and layer thickness.
机译:我们为海洋建模引入了混合的不连续/连续有限元对,具有连续的二次层厚度和不连续的速度。我们研究了应用于f平面上的线性浅水方程组的有限元对。元素对具有以下特性:所有强烈满足边界条件的地转平衡状态具有的离散散度恰好等于零,因此完全是离散方程的稳态。这意味着有限元对具有出色的地转平衡特性。我们还表明,应用于非旋转线性浅水方程组的元素对没有任何虚假的小特征值。我们使用数值测试说明了这些性质,并提供了收敛计算,这些数值计算表明数值解决方案的误差随速度和层厚随元件边缘长度的增加呈二次方衰减。

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