We performed one WEMVA pass with 10 conjugate-gradient solver
iterations on the ``WEMVA breaks'' dataset. In this instance the phase
differences caused by the velocity anomalies are too large to be
satisfactorily approximated in a Born manner. The velocity update
thus obtained is presented in Figure . It does not converge toward the true anomalies like the corresponding update in the upper panel of Figure
. Since this occurs when using the ideal image
perturbation, inaccuracies in extracting the perturbation would only amplify
the trend.
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There are several possible avenues for avoiding either the Born approximation limitations or the Born approximation altogether: 1. obtaining a very good velocity starting guess with other velocity analysis methods; 2. creating the image perturbation in connection with residual migration Sava and Biondi (2001); 3. employing linearizations other than Born Sava and Fomel (2002); 4. inverting for the lower frequencies first Pratt (1999); 5. using DSO WEMVA Sava and Symes (2002) where the image perturbation is extracted directly from the image using a specific operator during the inversion, without the need to find a corrected image.