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Echos get weaker with time, though the information content
is unrelated to the signal strength.
Echos also vary in strength as different materials are encountered
by the outgoing wave.
Programs for echo analysis typically divide the data by a scaling factor
that is a smoothed average of the signal strength.
This practice is nearly universal,
although it is fraught with hazards.
An example of automatic gain control (AGC)
is to compute the divisor by
forming the absolute value of the signal strength and then
smoothing with
the program triangle() or
the program leaky() .
Pitfalls are the strange amplitude behavior surrounding the water bottom,
and the overall loss of information contained in amplitudes.
Personally, I have found that the gain function t2 nearly always
eliminates the need for AGC on raw field data,
but I have no doubt that AGC is occasionally needed.
(A theoretical explanation for t2 is given in IEI.)
Next: Gain before or after
Up: WEIGHTED ERROR FILTERS
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Stanford Exploration Project
10/21/1998