(1) The optimum constant for the starting model is determined automatically.
(2) The weighted least-squares error between the predicted and measured traveltime data is as small as possible.
(3) The variance of the reconstructed slowness from the starting model is minimized.
(4) Rays with the greatest length have the least influence on the reconstructed slowness.
(5) Cells with most ray coverage tend to deviate least from the background value.
The resulting algorithm maps the reconstruction problem into a vector space where the contribution to the inversion from the background slowness remains invariant, while the optimum contributions in orthogonal directions are found. For a starting model with nonconstant slowness, the reconstruction algorithm has analogous properties.
J. S. Kallman and J. G. Berryman,
``Weighted
least-squares methods for electrical impedance tomography,''
IEEE Trans. Med. Imaging 11, 284-292 (1992).
I recommend getting a copy of this paper rather than the older one, unless you are not interested in any inversion problem except seismic.