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Joint time/frequency-domain inversion of reflection data for seabed geoacoustic profiles and uncertainties

机译:海底地声剖面和不确定性的反射数据联合时/频域反演

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This paper develops a joint time/frequency-domain inversion for high-resolution single-bounce reflection data, with the potential to resolve fine-scale profiles of sediment velocity, density, and attenuation over small seafloor footprints (similar to 100 m). The approach utilizes sequential Bayesian inversion of time- and frequency-domain reflection data, employing ray-tracing inversion for reflection travel times and a layer-packet stripping method for spherical-wave reflection-coefficient inversion. Posterior credibility intervals from the travel-time inversion are passed on as prior information to the reflection-coefficient inversion. Within the reflection-coefficient inversion, parameter information is passed from one layer packet inversion to the next in terms of marginal probability distributions rotated into principal components, providing an efficient approach to (partially) account for multi-dimensional parameter correlations with one-dimensional, numerical distributions. Quantitative geoacoustic parameter uncertainties are provided by a nonlinear Gibbs sampling approach employing full data error covariance estimation (including nonstationary effects) and accounting for possible biases in travel-time picks. Posterior examination of data residuals shows the importance of including data covariance estimates in the inversion. The joint inversion is applied to data collected on the Malta Plateau during the SCARAB98 experiment. (C) 2008 Acoustical Society of America.
机译:本文针对高分辨率的单反射反射数据开发了时域/频域联合反演方法,具有解决小规模海底足迹(约100 m)沉积物速度,密度和衰减的精细尺度分布的潜力。该方法利用时域和频域反射数据的顺序贝叶斯反演,将射线跟踪反演用于反射传播时间,并将层包剥离方法用于球面波反射系数反演。来自行进时间反演的后验可信区间作为先验信息传递给反射系数反演。在反射系数反演中,参数信息根据旋转到主成分的边际概率分布从一层数据包反演传递到下一层数据包反演,从而提供了一种有效的方法来(部分)说明一维的多维参数相关性,数值分布。非线性吉布斯采样方法提供了定量的地球声学参数不确定性,该方法采用了完整的数据误差协方差估计(包括非平稳效应)并考虑了行程时间选择中的可能偏差。对数据残差的后验表明,在反演中包括数据协方差估计的重要性。联合反演适用于SCARAB98实验期间在马耳他高原收集的数据。 (C)2008年美国声学学会。

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