Computational Modeling for High-Fidelity Coarsening of Shallow Water Equations Based on Subgrid Data

S. Ephrati, Erwin Luesink, G. Wimmer, P. Cifani, B. Geurts
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引用次数: 3

Abstract

Small-scale features of shallow water flow obtained from direct numerical simulation (DNS) with two different computational codes for the shallow water equations are gathered offline and subsequently employed with the aim of constructing a reduced-order correction. This is used to facilitate high-fidelity online flow predictions at much reduced costs on coarse meshes. The resolved small-scale features at high resolution represent subgrid properties for the coarse representation. Measurements of the subgrid dynamics are obtained as the difference between the evolution of a coarse grid solution and the corresponding DNS result. The measurements are sensitive to the particular numerical methods used for the simulation on coarse computational grids and can be used to approximately correct the associated discretization errors. The subgrid features are decomposed into empirical orthogonal functions (EOFs), after which a corresponding correction term is constructed. By increasing the number of EOFs in the approximation of the measured values the correction term can in principle be made arbitrarily accurate. Both computational methods investigated here show a significant decrease in the simulation error already when applying the correction based on the dominant EOFs only. The error reduction accounts for the particular discretization errors that incur and are hence specific to the particular simulation method that is adopted. This improvement is also observed for very coarse grids which may be used for computational model reduction in geophysical and turbulent flow problems.
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基于子网格数据的浅水方程高保真粗化计算建模
本文将直接数值模拟(DNS)得到的浅水流的小尺度特征与两种不同的浅水方程计算代码进行离线收集,然后用于构建降阶校正。这有助于高保真在线流量预测,大大降低了粗网格的成本。高分辨率的小尺度特征表示粗表示的子网格属性。子网格动力学的测量是通过粗网格解的演化与相应的DNS结果之间的差异来获得的。这些测量值对用于粗计算网格模拟的特定数值方法很敏感,可以用来近似地校正相关的离散化误差。将子网格特征分解为经验正交函数(EOFs),然后构造相应的校正项。通过增加测量值近似值中EOFs的数目,原则上可以使校正项变得任意精确。本文研究的两种计算方法都表明,当仅基于主导EOFs进行校正时,仿真误差已经显著降低。误差减少考虑了产生的特定离散化误差,因此是特定于所采用的特定模拟方法的。这种改进也适用于非常粗糙的网格,可用于地球物理和湍流问题的计算模型简化。
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