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Quantifying uncertainty in geoacoustic inversion. II. Application to broadband, shallow-water data

机译:量化地声反演中的不确定性。二。应用于宽带浅水数据

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This paper applies the new method of fast Gibbs sampling (FGS) to estimate the uncertainties of seabed geoacoustic parameters in a broadband, shallow-water acoustic survey, with the goal of interpreting the survey results and validating the method for experimental data. FGS applies a Bayesian approach to geoacoustic inversion based on sampling the posterior probability density to estimate marginal probability distributions and parameter covariances. This requires knowledge of the statistical distribution of the data errors, including both measurement and theory errors, which is generally not available. Invoking the simplifying assumption of independent, identically distributed Gaussian errors allows a maximum-likelihood estimate of the data variance and leads to a practical inversion algorithm. However, it is necessary to validate these assumptions, i.e., to verify that the parameter uncertainties obtained represent meaningful estimates. To this end, FGS is applied to a geoacoustic experiment carried out at a site off the west coast of Italy where previous acoustic and geophysical studies have been performed. The parameter uncertainties estimated via FGS are validated by comparison with : (i) the variability in the results of inverting multiple independent data sets collected during the experiment; (ii) the results of FGS inversion of synthetic test cases designed to simulate the experiment and data errors; and (iii) the available geophysical ground truth. Comparisons are carried out for a number of different source bandwidths, ranges, and levels of prior information, and indicate that FGS provides reliable and stable uncertainty estimates for the geoacoustic inverse problem.
机译:本文采用一种新的快速吉布斯采样法(FGS)来估计宽带浅水声调查中海床地声参数的不确定性,目的是解释调查结果并验证实验数据的方法。 FGS基于对后验概率密度进行采样以估计边际概率分布和参数协方差的贝叶斯方法对地声反演。这需要了解数据误差的统计分布,包括测量误差和理论误差,这通常是不可用的。调用独立的,相同分布的高斯误差的简化假设可以最大程度地估计数据方差,并得出一种实用的反演算法。但是,有必要验证这些假设,即验证所获得的参数不确定性代表有意义的估计。为此,将FGS应用于在意大利西海岸外的地点进行的地声实验,该地点以前已经进行过声学和地球物理研究。通过FGS估计的参数不确定性可通过与以下比较进行验证: (ii)旨在模拟实验和数据错误的综合测试用例的FGS反演结果; (iii)现有的地球物理地面真相。对许多不同的源带宽,范围和先验信息级别进行了比较,并表明FGS为地球声学反问题提供了可靠而稳定的不确定性估计。

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