Publication | Closed Access
Trans-dimensional geoacoustic inversion
159
Citations
35
References
2010
Year
AeroacousticsBayesian StatisticSeabed Reflection-coefficient DataEngineeringAppropriate Seabed StructureOceanographyMarkov Chain Monte CarloEarth ScienceUncertainty QuantificationBayesian MethodsComputational GeophysicsPublic HealthAcoustic Signal ProcessingStatisticsTrans-dimensional Geoacoustic InversionBayesian Hierarchical ModelingGeographyInverse Scattering TransformsInverse ProblemsInversion State SpaceSpeech ProcessingStatistical InferenceApproximate Bayesian Computation
This paper develops a general trans-dimensional Bayesian methodology for geoacoustic inversion. Trans-dimensional inverse problems are a generalization of fixed-dimensional inversion that includes the number and type of model parameters as unknowns in the problem. By extending the inversion state space to multiple subspaces of different dimensions, the posterior probability density quantifies the state of knowledge regarding inversion parameters, including effects due to limited knowledge about appropriate parametrization of the environment and error processes. The inversion is implemented here using a reversible-jump Markov chain Monte Carlo algorithm and the seabed is parametrized using a partition model. Unknown data errors are addressed by including a data-error model. Jumps between dimensions are implemented with a birth-death methodology that allows transitions between dimensions by adding or removing interfaces while maintaining detailed balance in the Markov chain. Trans-dimensional inversion results in an inherently parsimonious solution while partition modeling provides a naturally self-regularizing algorithm based on data information content, not on subjective regularization functions. Together, this results in environmental estimates that quantify appropriate seabed structure as supported by the data, allowing sharp discontinuities while approximating smooth transitions where needed. This approach applies generally to geoacoustic inversion and is illustrated here with seabed reflection-coefficient data.
| Year | Citations | |
|---|---|---|
Page 1
Page 1