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Model parameterization by spline

An accurate estimation of the gradient of the slowness field is necessary if we are to trace rays in a velocity model with high velocity contrast. Therefore, I have chosen to use cubic B-splines Inoue (1986) to parametrize the slowness model, which enables me to calculate the slowness gradient at an arbitrary point in the model. Another reason for using splines is that a wide variety of slowness models can be represented by a few spline coefficients. This means that the number of parameters in an optimization scheme that inverts for slowness can be reduced considerably.

The spline representation of a two-dimensional slowness model is  
 \begin{displaymath}
w (x_1,x_2) = \sum^N_{i=1} \sum^M_{j=1} c_{ij} F_i(x_1)G_j(x_2),\end{displaymath} (40)
with N and M the number of spline knots in the x1- and x2-direction. Fi and Gj are the spline functions at the ith knot in the x1-direction and the jth knot in the x2-direction, respectively.


next up previous print clean
Next: Inversion using the conjugate Up: Calculating the slowness error Previous: A system of ray
Stanford Exploration Project
2/5/2001