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A computational framework for infinite-dimensional Bayesian inverse problems. Part I: The linearized case, with application to global seismic inversion

机译:无限维贝叶斯逆的计算框架   问题。第一部分:线性化案例,适用于全球地震   逆温

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摘要

We present a computational framework for estimating the uncertainty in thenumerical solution of linearized infinite-dimensional statistical inverseproblems. We adopt the Bayesian inference formulation: given observational dataand their uncertainty, the governing forward problem and its uncertainty, and aprior probability distribution describing uncertainty in the parameter field,find the posterior probability distribution over the parameter field. The priormust be chosen appropriately in order to guarantee well-posedness of theinfinite-dimensional inverse problem and facilitate computation of theposterior. Furthermore, straightforward discretizations may not lead toconvergent approximations of the infinite-dimensional problem. And finally,solution of the discretized inverse problem via explicit construction of thecovariance matrix is prohibitive due to the need to solve the forward problemas many times as there are parameters. Our computational framework builds onthe infinite-dimensional formulation proposed by Stuart (A. M. Stuart, Inverseproblems: A Bayesian perspective, Acta Numerica, 19 (2010), pp. 451-559), andincorporates a number of components aimed at ensuring a convergentdiscretization of the underlying infinite-dimensional inverse problem. Theframework additionally incorporates algorithms for manipulating the prior,constructing a low rank approximation of the data-informed component of theposterior covariance operator, and exploring the posterior that together ensurescalability of the entire framework to very high parameter dimensions. Wedemonstrate this computational framework on the Bayesian solution of an inverseproblem in 3D global seismic wave propagation with hundreds of thousands ofparameters.
机译:我们提出了一个计算框架,用于估计线性化的无限维统计逆问题的数值解中的不确定性。我们采用贝叶斯推理公式:给定观测数据及其不确定性,控制正向问题及其不确定性,以及描述参数域中不确定性的先验概率分布,找到参数域中的后验概率分布。为了保证无限维反问题的适定性和便于后验计算,必须适当选择先验。此外,简单的离散化可能不会导致无穷维问题的收敛近似。最后,由于需要尽可能多地解决正向问题,因此无法通过协方差矩阵的显式构造来解决离散逆问题。我们的计算框架基于Stuart提出的无穷维公式(AM Stuart,《逆问题:贝叶斯观点》,Acta Numerica,19(2010),第451-559页),并纳入了许多旨在确保底层的收敛性离散化的组件。无限维反问题。框架还包含用于处理先验的算法,构造后协方差算子的数据通知组件的低秩近似,并探索可共同确保整个框架可缩放至非常高的参数尺寸的后验。在具有成千上万个参数的3D全球地震波传播的反问题的贝叶斯解决方案上演示该计算框架。

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