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Fast computation of uncertainty quantification measures in the geostatistical approach to solve inverse problems

机译:用地统计方法快速计算不确定性量化度量以解决反问题

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We consider the computational challenges associated with uncertainty quantification involved in parameter estimation such as seismic slowness and hydraulic transmissivity fields. The reconstruction of these parameters can be mathematically described as inverse problems which we tackle using the geostatistical approach. The quantification of uncertainty in the geostatistical approach involves computing the posterior covariance matrix which is prohibitively expensive to fully compute and store. We consider an efficient representation of the posterior covariance matrix at the maximum a posteriori (MAP) point as the sum of the prior covariance matrix and a low-rank update that contains information from the dominant generalized eigenmodes of the data misfit part of the Hessian and the inverse covariance matrix. The rank of the low-rank update is typically independent of the dimension of the unknown parameter. The cost of our method scales as O(m log m) where m dimension of unknown parameter vector space. Furthermore, we show how to efficiently compute measures of uncertainty that are based on scalar functions of the posterior covariance matrix. The performance of our algorithms is demonstrated by application to model problems in synthetic travel-time tomography and steady-state hydraulic tomography. We explore the accuracy of the posterior covariance on different experimental parameters and show that the cost of approximating the posterior covariance matrix depends on the problem size and is not sensitive to other experimental parameters. (C) 2015 Elsevier Ltd. All rights reserved.
机译:我们考虑与参数估算中涉及的不确定性量化相关的计算挑战,例如地震慢度和水力传输率场。这些参数的重建可以用数学方法描述为逆问题,我们可以使用地统计方法解决这些问题。地统计学方法中不确定性的量化涉及计算后协方差矩阵,而后者对于完全计算和存储来说是非常昂贵的。我们认为最大后验(MAP)点处的后协方差矩阵的有效表示形式是先验协方差矩阵和低秩更新的总和,该低秩更新包含来自Hessian数据不匹配部分的主要广义本征模信息的信息逆协方差矩阵。低等级更新的等级通常与未知参数的维数无关。我们方法的成本成O(m log m),其中m未知参数向量空间的维数。此外,我们展示了如何有效地计算基于后协方差矩阵的标量函数的不确定性度量。我们的算法的性能通过将其应用于合成行程层析成像和稳态液压层析成像中的模型问题得到了证明。我们探讨了后方协方差在不同实验参数上的准确性,并证明了近似后方协方差矩阵的成本取决于问题的大小,并且对其他实验参数不敏感。 (C)2015 Elsevier Ltd.保留所有权利。

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