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# SIGNAL-NOISE DECOMPOSITION BY DIP

Choose noise to be energy that has no spatial correlation and signal to be energy with spatial correlation consistent with one, two, or possibly a few plane-wave segments. (Another view of noise is that a huge number of plane waves is required to define the wavefield; in other words, with Fourier analysis you can make anything, signal or noise.) We know that a first-order differential equation can absorb (kill) a single plane wave, a second-order equation can absorb one or two plane waves, etc. In practice, we will choose the order of the wavefield and minimize power to absorb all we can, and call that the signal. is the operator that absorbs (by prediction error) the plane waves and absorbs noises and is a small scalar to be chosen. The difference between and is the spatial order of the filters. Because we regard the noise as spatially uncorrelated, has coefficients only on the time axis. Coefficients for are distributed over time and space. They have one space level, plus another level for each plane-wave segment slope that we deem to be locally present. In the examples here the number of slopes is taken to be two. Where a data field seems to require more than two slopes, it usually means the patch'' could be made smaller.

It would be nice if we could forget about the goal (10) but without it the goal (9), would simply set the signal equal to the data .Choosing the value of will determine in some way the amount of data energy partitioned into each. The last thing we will do is choose the value of ,and if we do not find a theory for it, we will experiment.

The operators and can be thought of as leveling'' operators. The method of least-squares sees mainly big things, and spectral zeros in and tend to cancel spectral lines and plane waves in and .(Here we assume that power levels remain fairly level in time. Were power levels to fluctuate in time, the operators and should be designed to level them out too.)

None of this is new or exciting in one dimension, but I find it exciting in more dimensions. In seismology, quasisinusoidal signals and noises are quite rare, whereas local plane waves are abundant. Just as a short one-dimensional filter can absorb a sinusoid of any frequency, a compact two-dimensional filter can absorb a wavefront of any dip.

To review basic concepts, suppose we are in the one-dimensional frequency domain. Then the solution to the fitting goals (10) and (9) amounts to minimizing a quadratic form by setting to zero its derivative, say
 (11)