Stochastic interpretation of magnetotelluric data, comparison of methods

Global optimization and stochastic approaches to the interpretation of measured data have recently gained particular
 attraction as tools for directed search for and/or verification of characteristic structural details and quantitative
 parameters of the deep structure, which is a ta...

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Main Authors: J. Pek, M. Menvielle, V. Cerv
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2007-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3084
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spelling doaj-baa542756a3d4e638fe91c143c8034f02020-11-25T02:02:13ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2007-06-0150110.4401/ag-3084Stochastic interpretation of magnetotelluric data, comparison of methodsJ. PekM. MenvielleV. CervGlobal optimization and stochastic approaches to the interpretation of measured data have recently gained particular
 attraction as tools for directed search for and/or verification of characteristic structural details and quantitative
 parameters of the deep structure, which is a task often arising when interpreting geoelectrical induction
 data in seismoactive and volcanic areas. We present a comparison of three common global optimization and stochastic
 approaches to the solution of a magnetotelluric inverse problem for thick layer structures, specifically the
 controlled random search algorithm, the stochastic sampling by the Monte Carlo method with Markov chains
 and its newly suggested approximate, but largely accelerated, version, the neighbourhood algorithm. We test the
 algorithms on a notoriously difficult synthetic 5-layer structure with two conductors situated at different depths,
 as well as on the experimental COPROD1 data set standardly used to benchmark 1D magnetotelluric inversion
 codes. The controlled random search algorithm is a fast and reliable global minimization procedure if a relatively
 small number of parameters is involved and a search for a single target minimum is the main objective of the
 inversion. By repeated runs with different starting test model pools, a sufficiently exhaustive mapping of the parameter
 space can be accomplished. The Markov chain Monte Carlo gives the most complete information for the
 parameter estimation and their uncertainty assessment by providing samples from the posterior probability distribution
 of the model parameters conditioned on the experimental data. Though computationally intensive, this
 method shows good performance provided the model parameters are sufficiently decorrelated. For layered models
 with mixed resistivities and layer thicknesses, where strong correlations occur and even different model classes
 may conform to the target function, the method often converges poorly and even very long chains do not guarantee
 fair distributions of the model parameters according to their probability densities. The neighbourhood resampling
 procedure attempts to accelerate the Monte Carlo simulation by approximating the computationally expensive
 true target function by a simpler, piecewise constant interpolant on a Voronoi mesh constructed over a
 set of pre-generated models. The method performs relatively fast but seems to suggest systematically larger uncertainties
 for the model parameters. The results of the stochastic simulations are compared with the standard
 linearized solutions both for thick layer models and for smooth Occam solutions.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3084magnetotelluric methodinverse problemcontrolled random searchMarkov chain Monte Carloneighbourhood algorithm
collection DOAJ
language English
format Article
sources DOAJ
author J. Pek
M. Menvielle
V. Cerv
spellingShingle J. Pek
M. Menvielle
V. Cerv
Stochastic interpretation of magnetotelluric data, comparison of methods
Annals of Geophysics
magnetotelluric method
inverse problem
controlled random search
Markov chain Monte Carlo
neighbourhood algorithm
author_facet J. Pek
M. Menvielle
V. Cerv
author_sort J. Pek
title Stochastic interpretation of magnetotelluric data, comparison of methods
title_short Stochastic interpretation of magnetotelluric data, comparison of methods
title_full Stochastic interpretation of magnetotelluric data, comparison of methods
title_fullStr Stochastic interpretation of magnetotelluric data, comparison of methods
title_full_unstemmed Stochastic interpretation of magnetotelluric data, comparison of methods
title_sort stochastic interpretation of magnetotelluric data, comparison of methods
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2007-06-01
description Global optimization and stochastic approaches to the interpretation of measured data have recently gained particular
 attraction as tools for directed search for and/or verification of characteristic structural details and quantitative
 parameters of the deep structure, which is a task often arising when interpreting geoelectrical induction
 data in seismoactive and volcanic areas. We present a comparison of three common global optimization and stochastic
 approaches to the solution of a magnetotelluric inverse problem for thick layer structures, specifically the
 controlled random search algorithm, the stochastic sampling by the Monte Carlo method with Markov chains
 and its newly suggested approximate, but largely accelerated, version, the neighbourhood algorithm. We test the
 algorithms on a notoriously difficult synthetic 5-layer structure with two conductors situated at different depths,
 as well as on the experimental COPROD1 data set standardly used to benchmark 1D magnetotelluric inversion
 codes. The controlled random search algorithm is a fast and reliable global minimization procedure if a relatively
 small number of parameters is involved and a search for a single target minimum is the main objective of the
 inversion. By repeated runs with different starting test model pools, a sufficiently exhaustive mapping of the parameter
 space can be accomplished. The Markov chain Monte Carlo gives the most complete information for the
 parameter estimation and their uncertainty assessment by providing samples from the posterior probability distribution
 of the model parameters conditioned on the experimental data. Though computationally intensive, this
 method shows good performance provided the model parameters are sufficiently decorrelated. For layered models
 with mixed resistivities and layer thicknesses, where strong correlations occur and even different model classes
 may conform to the target function, the method often converges poorly and even very long chains do not guarantee
 fair distributions of the model parameters according to their probability densities. The neighbourhood resampling
 procedure attempts to accelerate the Monte Carlo simulation by approximating the computationally expensive
 true target function by a simpler, piecewise constant interpolant on a Voronoi mesh constructed over a
 set of pre-generated models. The method performs relatively fast but seems to suggest systematically larger uncertainties
 for the model parameters. The results of the stochastic simulations are compared with the standard
 linearized solutions both for thick layer models and for smooth Occam solutions.
topic magnetotelluric method
inverse problem
controlled random search
Markov chain Monte Carlo
neighbourhood algorithm
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3084
work_keys_str_mv AT jpek stochasticinterpretationofmagnetotelluricdatacomparisonofmethods
AT mmenvielle stochasticinterpretationofmagnetotelluricdatacomparisonofmethods
AT vcerv stochasticinterpretationofmagnetotelluricdatacomparisonofmethods
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