Cg. Farquharson et Dw. Oldenburg, APPROXIMATE SENSITIVITIES FOR THE ELECTROMAGNETIC INVERSE PROBLEM, Geophysical journal international, 126(1), 1996, pp. 235-252
We present an approximate method for generating the Jacobian matrix of
sensitivities required by linearized, iterative procedures for invert
ing electromagnetic measurements. The approximation is based on the ad
joint-equation method in which the sensitivities are obtained by integ
rating, over each cell, the scalar product of an adjoint electric held
(the adjoint Green's function) with the electric held produced by the
forward modelling at the end of the preceding iteration. Instead of c
omputing the adjoint held in the multidimensional conductivity model,
we compute an approximate adjoint held, either in a homogeneous or lay
ered half-space. Such an approximate adjoint held is significantly fas
ter to compute than the true adjoint held. This leads to a considerabl
e reduction in computation time over the exact sensitivities. The spee
d-up can be one or two orders of magnitude, with the relative differen
ce increasing with the size of the problem. Sensitivities calculated u
sing the approximate adjoint held appear to be good approximations to
the exact sensitivities. This is verified by comparing true and approx
imate sensitivities for 2- and 3-D conductivity models, and for source
s that are both finite and infinite in extent. The approximation is su
fficiently accurate to allow an iterative inversion algorithm to conve
rge to the desired result, and we illustrate this by inverting magneto
telluric data to recover a 2-D conductivity structure. Our approximate
sensitivities should enable larger inverse problems to be solved than
is currently feasible using exact sensitivities and present-day compu
ting power.