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Variograms

A variogram is a function that quantifies spatial dependence of a random field Z across locations. The semivariogram gamma(h) is defined as gamma(h) = 1/2 E[(Z(x+h) - Z(x))^2], where h is a spatial lag. It describes how dissimilarity between observations increases with distance.

In practice, the empirical variogram is estimated from data by averaging squared differences of pairs separated

The variogram is tied to second-order stationarity; if the underlying field is second-order stationary or intrinsic,

Use in kriging: the fitted variogram (or its corresponding covariance model) is used to construct kriging weights,

Practical considerations include removing deterministic trends, ensuring adequate sampling geometry, handling outliers, and validating the model

by
lag
h:
gamma_hat(h)
=
(1/2N(h))
sum
[Z(x_i)
-
Z(x_i
+
h)]^2
over
all
pairs
with
separation
in
a
bin
around
h.
Key
features
are
the
sill
(the
plateau
value),
the
range
(the
distance
where
the
variogram
reaches
the
sill),
and
the
nugget
(the
value
at
h
approaching
zero,
often
indicating
measurement
error
or
microscale
variation).
the
variogram
exists
and
describes
the
dependence
structure.
Theoretical
models
often
fitted
to
empirical
variograms
include
spherical,
exponential,
Gaussian,
and
Matérn
forms,
characterized
by
parameters
such
as
nugget,
sill,
and
range.
Anisotropy
can
be
captured
by
directional
variograms,
which
are
computed
along
different
directions
to
reveal
varying
spatial
dependence.
enabling
optimal
spatial
interpolation
and
uncertainty
quantification.
The
variogram
thus
links
observed
data
to
predictions
at
unsampled
locations.
via
cross-validation.
Software
packages
commonly
implement
variogram
estimation,
model
fitting,
and
variogram-based
kriging.