RMfbm is an intrinsically stationary isotropic variogram
model. The corresponding centered semi-variogram only depends on the
distance $r \ge 0$ between two points and is given by
$$\gamma(r) = r^\alpha$$
where $\alpha \in (0,2]$.
By now, the model is implemented for dimensions up to 3.
For a generalized model see also RMgenfbm.
Usage
RMfbm(alpha, var, scale, Aniso, proj)
Arguments
alpha
parameter in $(0,2]$ refering to the RFfractaldimension of the
process
var,scale,Aniso,proj
optional parameters; same meaning for any
RMmodel. If not passed, the above
variogram remains unmodified.
The parameter $\alpha$ must satisfy $\alpha \in (0,2]$.
The variogram is unbounded and belongs to a non-stationary process with
stationary increments. For $\alpha=1$ and scale=2
we get a variogram corresponding to a standard Brownian Motion.
For $\alpha \in (0,2)$ the quantity $H =
\frac{\alpha} 2$ is called Hurst index and determines
the RFfractaldimension $D$ of the corresponding Gaussian sample paths
$$D = d + 1 - H$$
where $d$ is the dimension of the random field (see Chiles and
Delfiner, 1999, p. 89).
References
Chiles, J.-P. and P. Delfiner (1999)Geostatistics. Modeling
Spatial Uncertainty.New York, Chichester: John Wiley & Sons.
Stein, M.L. (2002) Fast and exact simulation of fractional
Brownian surfaces.J. Comput. Graph. Statist.11, 587--599