Backus–Gilbert method

In mathematics, the Backus–Gilbert method, also known as the optimally localized average (OLA) method is named for its discoverers, geophysicists

method, seek to impose smoothness constraints on the solution, Backus–Gilbert instead seeks to impose stability constraints, so that the solution would vary as little as possible if the input data were resampled multiple times. In practice, and to the extent that is justified by the data, smoothness results from this.

Given a data array X, the basic Backus-Gilbert inverse is:

${\displaystyle \mathbf {H} _{\theta }={\frac {\mathbf {C} ^{-1}\mathbf {G} _{\theta }}{\mathbf {G} _{\theta }^{T}\mathbf {C} ^{-1}\mathbf {G} _{\theta }}}}$

where C is the covariance matrix of the data, and G_θ is an a priori constraint representing the source θ for which a solution is sought. Regularization is implemented by "whitening" the covariance matrix:

${\displaystyle \mathbf {C} '=\mathbf {C} +\lambda \mathbf {I} }$

with C^′ replacing C in the equation for H_θ. Then,

${\displaystyle \mathbf {H} _{\theta }^{T}\mathbf {X} }$

is an estimate of the activity of the source θ.

References

• Backus, G.E., and Gilbert, F. 1968, "The Resolving power of Gross Earth Data",
  Geophysical Journal of the Royal Astronomical Society
  , vol. 16, pp. 169–205.
• Backus, G.E., and Gilbert, F. 1970, "Uniqueness in the Inversion of inaccurate Gross Earth Data", Philosophical Transactions of the Royal Society of London A, vol. 266, pp. 123–192.
• Press, WH; Teukolsky, SA; Vetterling, WT; Flannery, BP (2007). "Section 19.6. Backus–Gilbert Method".
  ISBN 978-0-521-88068-8. Archived from the original
  on 2011-08-11. Retrieved 2011-08-17.

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