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Distributed Implementation and Verification of Hybridizable Discontinuous Galerkin Methods for Nonhydrostatic Ocean Processes

机译:分布式实施和杂交不连续Galerkin方法的非水疗法海洋过程

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Nonhydrostatic, multiscale processes are an important part of our understanding of ocean dynamics. However, resolving these dynamics with traditional computational techniques can often be prohibitively expensive. We apply the hybridizable discontinuous Galerkin (HDG) finite element methodology to perform computationally efficient, high-order, nonhydrostatic ocean modeling by solving the Navier-Stokes equations with the Boussi-nesq approximation. In this work, we introduce a distributed implementation of our HDG projection method algorithm. We provide numerical experiments to verify our methodology using the method of manufactured solutions and provide preliminary benchmarking for our distributed implementation that highlight the advantages of the HDG methodology in the context of distributed computing. Lastly, we present simulations in which we capture nonhydrostatic internal waves that form as a result of tidal interactions with ocean topography. First, we consider the case of tidally-driven oscillatory flow over an abrupt, shallow seamount, and next, the case of strongly-stratified, oscillatory flow over a tall seamount. We analyze and compare our simulations to other results in literature.
机译:非水疗法,多尺度过程是我们对海洋动力学了解的重要组成部分。然而,用传统的计算技术解决这些动态通常可能是昂贵的。我们应用杂交的不连续的Galerkin(HDG)有限元方法,以通过用Boussi-nesq近似求解Navier-Stokes方程来执行计算效率,高阶的非水ratic海洋建模。在这项工作中,我们介绍了我们HDG投影方法算法的分布式实施。我们提供了使用制造解决方案方法验证我们的方法的数字实验,并为我们的分布式实施提供了初步基准,突出了在分布式计算的背景下突出了HDG方法的优势。最后,我们展示了我们捕获了由于与海洋地形的潮汐相互作用而形成的非水压内部波。首先,我们考虑在突然的,浅层海山和接下来的突然,浅层海山上的驱动振荡流动的情况,在高海山上有强烈的振荡流动的情况。我们分析并将模拟与文学中的其他结果进行比较。

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