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All subjects' data were entered into the inverse solution simultaneously in the SPM8 group inversion process, which results in a common source space across subjects.
We have run the inversion using a number of various initial guesses to see the most common inverse solution.
In Section 4, inverse solution techniques are summarized.
Sensitivity of inverse solution are studied and discussed.
The soil hydraulic parameters were optimized by inverse solution using the field data.
The inverse solution is obtained by pseudoinversion of the sensitivity matrix of relative amplitudes and phases.
The inverse solution of the broadband laser pulse with linear frequency chirp was also carried out.
The comparison between experimental and simulated results enables the Inverse Solution.
The bottom panel of Fig. 2 shows the final inverse solution obtained from the scheme.
The development of an alternative 3-D inverse solution is currently in progress.
To further suppress the ghost image, we introduce the approach of using the location inverse solution.
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