论文标题
使用高斯工艺仿真的非侵入性还原模型的潜在空间时间演变
Latent-space time evolution of non-intrusive reduced-order models using Gaussian process emulation
论文作者
论文摘要
非侵入性的还原模型(ROM)最近引起了人们对构建来自各个领域科学的非线性动力学系统的计算有效对应物的极大兴趣。它们为可能在本质上具有高维度的系统提供了低维的仿真框架。这是通过利用纯粹由数据驱动的构造算法来完成的。因此,毫不奇怪的是,机器学习的算法进步已导致不侵入性的ROM,其准确性和计算提高。但是,在绕过基于方程的进化的利用时,通常可以看出ROM框架的解释性受到影响。当使用黑盒深度学习方法时,这将变得更加问题,这些方法因在观察到的数据的物理状态之外缺乏鲁棒性而臭名昭著。在本文中,我们提出了基于高斯过程回归的新型潜在空间插值算法的使用。值得注意的是,系统的减少顺序演变是通过控制参数参数化的,以允许在空间中插值。此过程的使用还允许对时间进行连续解释,从而可以进行时间插值。后一个方面提供了有关全州进化的量化不确定性的信息,其分辨率比用于训练ROM的分辨率要精确。我们评估了该算法对Inviscid浅水方程式给出的以对流为主系统的可行性。
Non-intrusive reduced-order models (ROMs) have recently generated considerable interest for constructing computationally efficient counterparts of nonlinear dynamical systems emerging from various domain sciences. They provide a low-dimensional emulation framework for systems that may be intrinsically high-dimensional. This is accomplished by utilizing a construction algorithm that is purely data-driven. It is no surprise, therefore, that the algorithmic advances of machine learning have led to non-intrusive ROMs with greater accuracy and computational gains. However, in bypassing the utilization of an equation-based evolution, it is often seen that the interpretability of the ROM framework suffers. This becomes more problematic when black-box deep learning methods are used which are notorious for lacking robustness outside the physical regime of the observed data. In this article, we propose the use of a novel latent-space interpolation algorithm based on Gaussian process regression. Notably, this reduced-order evolution of the system is parameterized by control parameters to allow for interpolation in space. The use of this procedure also allows for a continuous interpretation of time which allows for temporal interpolation. The latter aspect provides information, with quantified uncertainty, about full-state evolution at a finer resolution than that utilized for training the ROMs. We assess the viability of this algorithm for an advection-dominated system given by the inviscid shallow water equations.