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光滑性及其他超参数估计与数据同化相关反问题

Smoothness and other hyperparameter estimation for inverse problems related to data assimilation

Imperial College, London(伦敦帝国理工学院)

Baptiste Simandoux, Nikolas Kantas, Dan Crisan

AI总结:

本文研究数据同化中动力系统部分微分方程反问题的贝叶斯逆问题,重点探讨光滑性等超参数的联合估计方法,通过高维Metropolis-within-Gibbs采样实现后验推断,验证了联合估计在不确定性量化和参数估计中的有效性。

摘要:

我们考虑数据同化中由偏微分方程和随机偏微分方程支配的动力系统所出现的贝叶斯逆问题。时空依赖场与先验和似然密度的静态参数联合推断。特别强调控制先验光滑性和正则性的超参数,这对确保问题良好设定、塑造后验结构和确定预测不确定性至关重要。通常假设该超参数已知且固定;然而在本文中,我们采用分层贝叶斯框架,将光滑性和其他超参数视为未知并分配超先验。后验推断通过适用于高维空间的Metropolis-within-Gibbs采样进行,其中超参数估计计算开销很小。该方法在Navier-Stokes方程和随机对流-扩散方程的反问题中得到验证,使用不同协方差结构的高斯先验,在稀疏和密集观测情况下进行测试。数值结果表明,联合估计光滑性显著减少了由光滑性误指定引起的不确定性量化和参数估计误差,其性能与真实光滑性已知的情况相当。

英文摘要:

We consider Bayesian inverse problems arising in data assimilation for dynamical systems governed by partial and stochastic partial differential equations. The space-time dependent field is inferred jointly with static parameters of the prior and likelihood densities. Particular emphasis is placed on the hyperparameter controlling the prior smoothness and regularity, which is critical in ensuring well-posedness, shaping posterior structure, and determining predictive uncertainty. Commonly it is assumed to be known and fixed a priori; however in this paper we will adopt a hierarchical Bayesian framework in which smoothness and other hyperparameters are treated as unknown and assigned hyperpriors. Posterior inference is performed using Metropolis-within-Gibbs sampling suitable to high dimensions, for which hyperparameter estimation involves little computational overhead. The methodology is demonstrated on inverse problems for the Navier-Stokes equations and the stochastic advection-diffusion equation, under sparse and dense observation regimes, using Gaussian priors with different covariance structure. Numerical results show that jointly estimating the smoothness substantially reduces the errors in uncertainty quantification and parameter estimation induced by smoothness misspecification, by achieving performance comparable to scenarios in which the true smoothness is known.

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