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Reformulation of Bayesian Geostatistical Approach on Principal Components

机译:贝叶斯地统计方法对主要成分的重新制定

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摘要

In this note, we reformulate Bayesian geostatistical inverse approach based on principal component analysis of the spatially correlated parameter field to be estimated. The unknown parameter field is described by a latent-variable model as a realization of projections on its principal component axes. The reformulated geostatistical approach (RGA) achieves substantial dimensionality reduction by estimating the latent variable of projections on truncated principal components instead of directly estimating the parameter field. We provide solutions for best estimates and posterior variances for linear and quasi-linear inverse problems. The number of normal equations to be solved is reduced to k+p, where k is the number of retained principal components and p is the number of drifts, both independent of the number of observations. To determine the Jacobian matrix for quasi-linear problems, the number of forward model runs in each iteration is reduced to k+p+1. There is no need to evaluate the Jacobian matrix in terms of the unknown parameter field. RGA unifies the problem setup and computational techniques for large-dimensional inverse problems introduced previously, which are now naturally built in the reformulated framework. RGA is more efficient and scalable for both large-dimensional inverse problems and problems with a massive volume of observations. Moreover, conditional realizations of the parameter field can be conveniently generated by generating conditional realizations of latent variables on truncated principal component axes. We also relate the new approach to the classical geostatistical approach formulas. Large-dimensional hydraulic tomography problems are used to demonstrate the application of the reformulated approach.Key PointsBayesian geostatistical approach is reformulated to estimate projections on principal component axes and generate conditional realizations The new framework unifies inverse problem setup and computational techniques for large-dimensional inverse problems Both forward model runs and normal equations are reduced to the number of retained principal components, providing high scalability
机译:在本说明书中,我们根据要估计的空间相关参数场的主成分分析来重整贝叶斯地质统计逆方法。未知参数字段由潜在变量模型描述为其主组件轴上的投影的实现。通过估计截断的主成分上的投影的潜变量而不是直接估计参数字段,重新稳定的地质统计方法(RGA)实现了大量的维度减少。我们为线性和准线性逆问题提供最佳估计和后域的解决方案。要解决的正常方程的数量减少到k + p,其中k是保留的主成分的数量,并且P是漂移的数量,无论是无关的观察数。为了确定准线性问题的雅可比矩阵,每次迭代中的前向模型的数量减少到k + p + 1。在未知的参数字段中,无需评估雅可比矩阵。 RGA统一以前引入的大维逆问题的问题设置和计算技术,现在在重新制定的框架中自然地构建。 RGA对于大维逆问题和大量观测的问题更有效和可扩展。此外,可以通过在截短的主分量轴上生成潜伏变量的条件实现来方便地生成参数字段的条件实现。我们还涉及经典地稳态统计方法公式的新方法。大维液压断层扫描问题用于证明重新制定方法的应用。重新重新重新重新稳定地统计方法以估算主成分轴的预测,并生成条件实现新框架统一的逆问题设置和用于大维逆问题的计算技术的预制转发模型运行和正常方程都减少到保留的主组件的数量,提供高可伸缩性

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