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7.9 Geostatistics (by R. Gebbers)                               173

             ZID = ZI;
             ZID(find(ZID > 20)) = NaN;
             contourf(XI,YI,ZID,v)
             caxis([-40 40]), colorbar, hold on
             plot(data(:,1),data(:,2),'ko')
             text(data(:,1)+1,data(:,2),labels)
           Alternatively, we can eliminate a rectangular area with no data.

             ZID = ZI;
             ZID(131:201,1:71) = NaN;

             contourf(XI,YI,ZID,v)
             caxis([-40 40]), colorbar, hold on
             plot(data(:,1),data(:,2),'ko')
             text(data(:,1)+1,data(:,2),labels)

           In some examples, the area with no control points is simply eliminated by
           putting a legend on this part of the map.
             MATLAB provides a number of other gridding techniques. Another very
           useful MATLAB gridding method are  splines with tension by Wessel and
           Bercovici (1998). The  tsplines use biharmonic splines in tension t, where
           the parameter t can vary between 0 and 1. A value of t=0 corresponds to a
           standard cubic spline interpolation. Increasing t reduces undesirable oscil-
           lations between data points, e.g., the paired lows and highs observed in one
           of the above examples. The limiting situation t|1 corresponds to linear
           interpolation.



           7.9 Geostatistics (by R. Gebbers)

           Geostatistics is used to describe the autocorrelation of one or more variables
           in the 1D, 2D, and 3D space or even in 4D space-time, to make predic-
           tions at unobserved locations, to give information about the accuracy of
           prediction and to reproduce spatial variability and uncertainty. The shape,
           the range, and the direction of the spatial autocorrelation is described by
           the variogram, which is the main tool in linear geostatistics. The origins
           of geostatistics can be dated back to the early 50·s when the South African

           mining engineer Daniel G. Krige first published an interpolation method
           based on spatial dependency of samples. In the 60·s and 70·s, the French
           mathematician George Matheron developed the  theory of  regionalized vari-
           ables which provides the theoretical foundations of Kriges·s more practical
           methods. This theory forms the basis of several procedures for the analysis
           and estimation of spatially dependent variables, which Matheron called geo-
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