Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions

A goal of geophysical inversion is to identify all models which give an acceptable misfit between predicted and observed data. However, because of the complexity of Earth structure, the non-linearity of physical processes in the Earth, and the insufficiency of geophysical data, many geophysical inve...

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Main Authors: A. Lomax, R. Snieder
Format: Article
Language:English
Published: Copernicus Publications 1995-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/2/222/1995/npg-2-222-1995.pdf
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spelling doaj-d51668d1c37a4eeaa8e482e4b1f9db312020-11-24T22:59:32ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79461995-01-0123/4222227Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functionsA. LomaxR. SniederA goal of geophysical inversion is to identify all models which give an acceptable misfit between predicted and observed data. However, because of the complexity of Earth structure, the non-linearity of physical processes in the Earth, and the insufficiency of geophysical data, many geophysical inverse problems may have a large number of distinct, acceptable solutions. These problems may be characterized by a complicated surface for the misfit function in the solution parameter space. For exploring such a surface, direct inversion and simple random search methods are often inadequate. However, directed search methods such as the genetic algorithm can be configured to balance convergent and random processes to find large sets of solutions that span the acceptable regions of complicated misfit surfaces.http://www.nonlin-processes-geophys.net/2/222/1995/npg-2-222-1995.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Lomax
R. Snieder
spellingShingle A. Lomax
R. Snieder
Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
Nonlinear Processes in Geophysics
author_facet A. Lomax
R. Snieder
author_sort A. Lomax
title Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
title_short Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
title_full Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
title_fullStr Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
title_full_unstemmed Identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
title_sort identifying sets of acceptable solutions to non-linear, geophysical inverse problems which have complicated misfit functions
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 1995-01-01
description A goal of geophysical inversion is to identify all models which give an acceptable misfit between predicted and observed data. However, because of the complexity of Earth structure, the non-linearity of physical processes in the Earth, and the insufficiency of geophysical data, many geophysical inverse problems may have a large number of distinct, acceptable solutions. These problems may be characterized by a complicated surface for the misfit function in the solution parameter space. For exploring such a surface, direct inversion and simple random search methods are often inadequate. However, directed search methods such as the genetic algorithm can be configured to balance convergent and random processes to find large sets of solutions that span the acceptable regions of complicated misfit surfaces.
url http://www.nonlin-processes-geophys.net/2/222/1995/npg-2-222-1995.pdf
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AT rsnieder identifyingsetsofacceptablesolutionstononlineargeophysicalinverseproblemswhichhavecomplicatedmisfitfunctions
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