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Journal ArticleDOI

Generalized Nonlinear Inverse Problems Solved Using the Least Squares Criterion

Albert Tarantola, +1 more
- 01 May 1982 - 
- Vol. 20, Iss: 2, pp 219-232
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TLDR
In this article, a general definition of the nonlinear least squares inverse problem is given, where the form of the theoretical relationship between data and unknowns may be general (in particular, nonlinear integrodierentia l equations).
Abstract
We attempt to give a general definition of the nonlinear least squares inverse problem. First, we examine the discrete problem (finite number of data and unknowns), setting the problem in its fully nonlinear form. Second, we examine the general case where some data and/or unknowns may be functions of a continuous variable and where the form of the theoretical relationship between data and unknowns may be general (in particular, nonlinear integrodierentia l equations). As particular cases of our nonlinear algorithm we find linear solutions well known in geophysics, like Jackson’s (1979) solution for discrete problems or Backus and Gilbert’s (1970) a solution for continuous problems.

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Citations
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Journal ArticleDOI

Regional tomographic inversion of the amplitude and phase of Rayleigh waves with 2-D sensitivity kernels

TL;DR: In this paper, a 2D sensitivity kernel for fundamental-mode Rayleigh waves based on the single-scattering (Born) approximation was proposed to account for the effects of heterogeneous structure on the wavefield in a regional surface wave study.
Journal ArticleDOI

Anisotropy and shear-velocity heterogeneities in the upper mantle

TL;DR: In this article, a long-period surface wave is used to map lateral heterogeneities of velocity and anisotropy in the upper mantle and the dispersion curves are expanded in spherical harmonics up to degree 6 and inverted to find the depth structure.
Journal ArticleDOI

A correlation-based misfit criterion for wave-equation traveltime tomography

TL;DR: In this article, the authors proposed an alternative criterion to measure the relative phase shift, which is a weighted norm of the correlation and is less sensitive to differences in the amplitude spectra.
Journal ArticleDOI

Three‐dimensional elastic wave velocity structure of the western and central Tien Shan

TL;DR: In this article, the authors used the arrival times of compressional (P) and shear (S) waves generated by earthquakes at local and teleseismic distances and recorded by seismographs located in the western and central Tien Shan are used to determine one-and three-dimensional elastic wave velocity structures of the crust and upper mantle beneath the mountain belt.
Journal ArticleDOI

A New Vector Waveform Inversion Algorithm for Simultaneous Updating of Conductivity and Permittivity Parameters From Combination Crosshole/Borehole-to-Surface GPR Data

TL;DR: An iterative gradient method in which the steepest descent direction, used to update iteratively the permittivity and conductivity distributions in an optimal way, is found by cross-correlating the forward vector wavefield and the backward-propagated vectorial residual wavefield.
References
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Book

Linear statistical inference and its applications

TL;DR: Algebra of Vectors and Matrices, Probability Theory, Tools and Techniques, and Continuous Probability Models.
Journal ArticleDOI

Uniqueness in the Inversion of Inaccurate Gross Earth Data

TL;DR: In this article, it was shown that a given set G of measured gross Earth data permits such a construction of localized averages, and if so, how to find the shortest length scale over which G gives a local average structure at a particular depth if the variance of the error in computing that local average from G is to be less than a specified amount.
Journal ArticleDOI

The general linear inverse problem - Implication of surface waves and free oscillations for earth structure.

TL;DR: In this paper, the discrete general linear inverse problem is reduced to a set of m equations in n unknowns and a linear combination of the eigenvectors of the coefficient matrix can be used to determine parameter resolution and information distribution among the observations.