论文标题

Fokker-Planck方程的概率流解决方案

Probability flow solution of the Fokker-Planck equation

论文作者

Boffi, Nicholas M., Vanden-Eijnden, Eric

论文摘要

在高维度中整合时间依赖性的fokker-planck方程的选择方法是通过集成相关的随机微分方程来从溶液中生成样品。在这里,我们研究了一种基于整合了描述概率流的普通微分方程的替代方案。该方程充当传输图,可以确定地将样品从初始密度从溶液中的样品推到了任何以后的时间。与随机动力学的整合不同,该方法具有直接访问数量的优势,这些数量挑战仅凭轨迹,例如概率电流,密度本身及其熵。概率流程方程取决于溶液对数的梯度(其“得分”),因此A-Priori未知也是如此。为了解决这一依赖性,我们通过根据瞬时概率电流传播一组样本来在直接学习的深度神经网络中对分数进行建模。从理论上讲,我们表明所提出的方法控制了KL从学习溶液到目标的差异,而从随机微分方程中学习的外部样本并不能控制KL差异的任何一个方向。从经验上讲,我们考虑了相互作用粒子系统物理学的几个高维fokker-planck方程。我们发现,该方法在可用的分析解决方案以及通过蒙特卡洛(Monte-Carlo)计算时的矩时准确匹配。此外,该方法为全球熵产生速率提供了令人信服的预测,这些预测超过了从随机轨迹学习中获得的表现,并且可以有效地捕获长时间间隔内的非平衡稳态概率电流。

The method of choice for integrating the time-dependent Fokker-Planck equation in high-dimension is to generate samples from the solution via integration of the associated stochastic differential equation. Here, we study an alternative scheme based on integrating an ordinary differential equation that describes the flow of probability. Acting as a transport map, this equation deterministically pushes samples from the initial density onto samples from the solution at any later time. Unlike integration of the stochastic dynamics, the method has the advantage of giving direct access to quantities that are challenging to estimate from trajectories alone, such as the probability current, the density itself, and its entropy. The probability flow equation depends on the gradient of the logarithm of the solution (its "score"), and so is a-priori unknown. To resolve this dependence, we model the score with a deep neural network that is learned on-the-fly by propagating a set of samples according to the instantaneous probability current. We show theoretically that the proposed approach controls the KL divergence from the learned solution to the target, while learning on external samples from the stochastic differential equation does not control either direction of the KL divergence. Empirically, we consider several high-dimensional Fokker-Planck equations from the physics of interacting particle systems. We find that the method accurately matches analytical solutions when they are available as well as moments computed via Monte-Carlo when they are not. Moreover, the method offers compelling predictions for the global entropy production rate that out-perform those obtained from learning on stochastic trajectories, and can effectively capture non-equilibrium steady-state probability currents over long time intervals.

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