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arXiv 2012.00638physics.flu-dyncs.NAmath.NA
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准地转方程的降阶模式:简要综述

Reduced Order Models for the Quasi-Geostrophic Equations: A Brief Survey

Changhong Mou, Zhu Wang, David R. Wells, Xuping Xie, Traian Iliescu

摘要:

降阶模型(ROM)是其维度显著低于通过经典数值离散化获得的那些维度的计算模型(例如,有限元、有限差分、有限体积或谱方法)。因此,ROM已经被用于加速许多查询问题的数值模拟,例如,不确定性量化、控制和形状优化。基于投影的ROM在流体流动的数值模拟中特别成功。在这篇简短的综述中,我们总结了准地转方程(QGE)(也称为正压涡度方程)的一些最新ROM发展,这是一个简化的地球物理流模型,其中旋转起着核心作用,如风驱动的海洋环流在中纬度海洋盆地。由于QGE代表了有效的数值模拟海洋流动和大尺度海洋动力学的准确表示之间的实际折衷,这些方程经常被用于测试新的数值方法的海洋流动。ROM还在QGE上进行了各种设置的测试,以了解它们在有效的海洋流动数值模拟中的潜力。在本文中,我们调查了为QGE开发的ROM,以了解它们在更复杂的海洋流动的有效数值模拟中的潜力:我们解释了如何使用经典的QGE数值方法来生成ROM基函数,我们概述了构建基于投影的ROM的主要步骤(特别关注欠解析区域,当需要解决闭合问题时),我们说明了各种设置下QGE数值模拟中的ROM,我们提出了几个潜在的未来研究途径,在ROM勘探的QGE和更复杂的模型的地球物理流。

英文摘要:

Reduced order models (ROMs) are computational models whose dimension is significantly lower than those obtained through classical numerical discretizations (e.g., finite element, finite difference, finite volume, or spectral methods). Thus, ROMs have been used to accelerate numerical simulations of many query problems, e.g., uncertainty quantification, control, and shape optimization. Projection-based ROMs have been particularly successful in the numerical simulation of fluid flows. In this brief survey, we summarize some recent ROM developments for the quasi-geostrophic equations (QGE) (also known as the barotropic vorticity equations), which are a simplified model for geophysical flows in which rotation plays a central role, such as wind-driven ocean circulation in mid-latitude ocean basins. Since the QGE represent a practical compromise between efficient numerical simulations of ocean flows and accurate representations of large scale ocean dynamics, these equations have often been used in the testing of new numerical methods for ocean flows. ROMs have also been tested on the QGE for various settings in order to understand their potential in efficient numerical simulations of ocean flows. In this paper, we survey the ROMs developed for the QGE in order to understand their potential in efficient numerical simulations of more complex ocean flows: We explain how classical numerical methods for the QGE are used to generate the ROM basis functions, we outline the main steps in the construction of projection-based ROMs (with a particular focus on the under-resolved regime, when the closure problem needs to be addressed), we illustrate the ROMs in the numerical simulation of the QGE for various settings, and we present several potential future research avenues in the ROM exploration of the QGE and more complex models of geophysical flows.

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