| RMcoxisham {RandomFields} | R Documentation |
RMcoxisham is a stationary covariance model
which depends on a univariate stationary isotropic covariance model
C_0, which is a normal scale mixture.
The corresponding covariance function only depends on the difference
(h,t) \in {\bf R}^{d+1}={\bf R}^d\times{\bf R} between two points in d+1-dimensional space and is given by
C(h,t)=|E + t^\beta D|^{-1/2} C_0([(h - t \mu)^T (E + t^\beta
D)^{-1} (h - t \mu)]^{1/2})
Here \mu \in {\bf R}^d is a vector in
d-dimensional space;
E is the d \times d-identity matrix and D is
a d \times d-correlation matrix with |D| > 0.
The parameter \beta is in (0,2].
Currently, the implementation is done only for d=2.
RMcoxisham(phi,mu,D,beta,var, scale, Aniso, proj)
phi |
a univariate stationary isotropic covariance model for random fields
on |
mu |
a vector in |
D |
a |
beta |
numeric in the interval |
var, scale, Aniso, proj |
optional arguments; same meaning for any
|
This model stems from a rainfall model (cf. Cox, D.R., Isham, V.S. (1988)) and equals the following expectation
C(h,t)=\bold{E}_V C_0(h-Vt)
where the random wind speed vector V follows a d-variate
normal distribution with expectation mu and covariance matrix D/2
(cf. Schlather, M. (2010), Example 9).
RMcoxisham returns an object of class RMmodel.
Martin Schlather, schlather@math.uni-mannheim.de, https://www.wim.uni-mannheim.de/schlather/
Cox, D.R., Isham, V.S. (1988) A simple spatial-temporal model of rainfall. Proc. R. Soc. Lond. A, 415, 317-328.
Schlather, M. (2010) On some covariance models based on normal scale mixtures. Bernoulli, 16, 780-797.
RFoptions(seed=0) ## *ANY* simulation will have the random seed 0; set
## RFoptions(seed=NA) to make them all random again
model <- RMcoxisham(RMgauss(), mu=1, D=1)
x <- seq(0, 10, 0.3)
plot(model, dim=2)
plot(RFsimulate(model, x=x, y=x))