Geophysical inversion with a neighbourhood algorithm - II. Appraising the ensemble

Authors
Citation
M. Sambridge, Geophysical inversion with a neighbourhood algorithm - II. Appraising the ensemble, GEOPHYS J I, 138(3), 1999, pp. 727-746
Citations number
50
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICAL JOURNAL INTERNATIONAL
ISSN journal
0956540X → ACNP
Volume
138
Issue
3
Year of publication
1999
Pages
727 - 746
Database
ISI
SICI code
0956-540X(199909)138:3<727:GIWANA>2.0.ZU;2-8
Abstract
Monte Carlo direct search methods, such as genetic algorithms, simulated an nealing, etc., are often used to explore a finite-dimensional parameter spa ce. They require the solving of the forward problem many times, that is, ma king predictions of observables from an earth model. The resulting ensemble of earth models represents all 'information' collected in the search proce ss. Search techniques have been the subject of much study in geophysics; le ss attention is given to the appraisal of the ensemble. Often inferences ar e based on only a small subset of the ensemble, and sometimes a single memb er. This paper presents a new approach to the appraisal problem. To our knowled ge this is the first time the general case has been addressed, that is, how to infer information from a complete ensemble, previously generated by any search method. The essence of the new approach is to use the information i n the available ensemble to guide a resampling of the parameter space. This requires no further solving of the forward problem, but from the new 'resa mpled' ensemble we are able to obtain measures of resolution and trade-off in the model parameters, or any combinations of them. The new ensemble inference algorithm is illustrated on a highly non-linear waveform inversion problem. wt is shown how the computation time and memory requirements scale with the dimension of the parameter space and size of t he ensemble. The method is highly parallel, and may easily be distributed a cross several computers. Since little is assumed about the initial ensemble of earth models, the technique is applicable to a wide variety of situatio ns. For example, it may be applied to perform 'error analysis' using the en semble generated by a genetic algorithm, or any other direct search method.