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If system (3) produces track-free maps, the skeptic might wonder, why
even bother directly estimating the systematic error in the data? First, as mentioned
earlier, system (3) leads to a loss of resolution in the final map.
Second, in many cases we may have prior information about the distribution and magnitude
of the systematic error, which we could then include as an ``inverse model covariance''
(regularization operator) in system (4).
By directly estimating and subtracting systematic errors, we have more faith that the final map is an
accurate representation of the true quantity. While the authors of the previously mentioned
papers on Galilee and Madagascar were more interested in resolving the topographical features
than the value of the underlying field, in many applications, the field itself is most important.
Furthermore, when the systematic error is explainable by physical or other phenomena, we want to
have control in its estimation.
Next: Building a map with
Up: Methodology
Previous: Estimation of systematic error
Stanford Exploration Project
9/18/2001