The examples above assume that each variable
has it's
own unique parameter vector
.
It is however possible to
define common parameters for multiple variables (with
merge). It is for instance
possible to define a common mean (intercept) (see ``standardised ordinary
cokriging'' in [8, p. 70], [12, p. 409-416],
or [10, p. 323], or ``collocated cokriging''
[10, p. 326]), or to define a common regressor across
different variables (cf. Analysis of covariance models, [3, p. 193
and excercise 9.1]). In any case,
and
loose their typical block structure. For instance, with
,
and the trend of both
and
consist of one single
intercept (merging the intercept for both variables) leads to an
matrix with only one column, filled with ones.
When the residuals are not correlated and have unequal variance, i.e. under
the model
Least squares predictions at location
are obtained by
When common parameters are defined with merge, and no variograms are specified, then estimation and prediction under the OLS and WLS models will be done, in which case the constant variance is assumed for the joint (multivariable) residual. In this case, known ratios in variances between different variables can still be set using the V field of each data variable.
Known, constant measurement error can be defined in the variogram model.
Suppose the variable
has an apparent nugget effect of 1 and a
spatially correlated part of 1 exp(10), than the variogram model can
be written as 1 Nug() + 1 Exp(10). This would yield the `standard'
kriging predictions, i.e. exact interpolation. If it is known that 75%
of the nugget variance constitues of measurement error, and predictions
are required for the measurement error free part of the variable, then
the variogram of
can be defined as:
variogram(y): 0.75 Err() + 0.25 Nug() + 1 Exp(10)
see for more information [5].
Known, varying measurement errors can be defined (for data in
column files) by specifying the V field. When variograms are
specified and the goal is prediction or trend prediction, then the
covariances
are taken to be
,
with
the value
of the V-field of record
,
thus interpreting the variance
field (V) as a known, location-specific measurement error
[7,20,5]. Otherwise formulated: in this
case
is used as covariance matrix, instead of
only. Putting
a constant in the V field should yield the same results as
specifying this value in the Err term of the variogram.