Hi Carlo,
Note that a sill strongly different from 1 would
mean that the assumption of 2nd order stationarity
underlying SGS is not met.
I wouldn't force the sill to be one when
fitting the model and you have to use a unit sill
model in the simulation program for consistency.
If the deviation
Hi.
I want to use Ordinary Kriging on
an arbitrary dataset of X,Y, and Z values to estimate the
Z values on a grid of arbitrary size/density. But I dont know what
length and scale parameters to choose for the semivariogram.
So I need to answer the following questions. Im looking for
