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Dimension reduction for integrating data series in Bayesian inversion of geostatistical models

机译:在地统计模型的贝叶斯反演中整合数据系列的维度减少

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摘要

This study explores methods with which multidimensional data, e.g. time series, can be effectively incorporated into a Bayesian framework for inferring geostatistical parameters. Such series are difficult to use directly in the likelihood estimation procedure due to their high dimensionality; thus, a dimension reduction approach is taken to utilize these measurements in the inference. Two synthetic scenarios from hydrology are explored in which pumping drawdown and concentration breakthrough curves are used to infer the global mean of a log-normally distributed hydraulic conductivity field. Both cases pursue the use of a parametric model to represent the shape of the observed time series with physically-interpretable parameters (e.g. the time and magnitude of a concentration peak), which is compared to subsets of the observations with similar dimensionality. The results from both scenarios highlight the effectiveness for the shape-matching models to reduce dimensionality from 100+ dimensions down to less than five. The models outperform the alternative subset method, especially when the observations are noisy. This approach to incorporating time series observations in the Bayesian framework for inferring geostatistical parameters allows for high-dimensional observations to be faithfully represented in lower-dimensional space for the non-parametric likelihood estimation procedure, which increases the applicability of the framework to more observation types. Although the scenarios are both from hydrogeology, the methodology is general in that no assumptions are made about the subject domain. Any application that requires the inference of geostatistical parameters using series in either time of space can use the approach described in this paper.
机译:本研究探讨了多维数据,例如多维数据的方法。时间序列,可以有效地纳入贝叶斯框架中,用于推断地质统计参数。由于其高维度,这种系列难以直接在可能的估计过程中使用;因此,采用尺寸减少方法来利用推理中的这些测量。探索了一种来自水文的两个合成情景,其中泵送拔展和浓度突破性曲线用于推断对数常数分布的液压导电场的全局平均值。这两种情况都追求使用参数模型来表示观察时间序列的形状与物理解释的参数(例如,浓度峰的时间和大小)与具有相似维度相似的观察的子集进行比较。这两种情况的结果突出了形状匹配模型的有效性,以将维度从100+维度降低到小于五个。该模型优于替代的子集方法,尤其是观察噪声时。在贝叶斯框架中结合时间序列观测的这种方法,用于推断地质统计参数允许在非参数似然估计过程的较低尺寸空间中忠实地表示的高维观察,这增加了框架对更多观察类型的适用性。虽然这种情况既来自水文地质学,则方法是一般的,因为没有关于主题领域的假设。任何需要在空间中使用串的序列都可以使用本文中描述的方法的任何应用。

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