RMbessel is a stationary isotropic covariance model
belonging to the Bessel family.
The corresponding covariance function only depends on the distance $r \ge 0$ between
two points and is given by
$$C(r) = 2^\nu \Gamma(\nu+1) r^{-\nu} J_\nu(r)$$
where $\nu \ge \frac{d-2}2$,
$\Gamma$ denotes the gamma function and
$J_\nu$ is a Bessel function of first kind.
Usage
RMbessel(nu, var, scale, Aniso, proj)
Arguments
nu
a numerical value; should be equal to or greater than
$\frac{d-2}2$ to provide a valid
covariance function for a random field of dimension $d$.
var,scale,Aniso,proj
optional parameters; same meaning for any
RMmodel. If not passed, the above
covariance function remains unmodified.
This covariance models a hole effect (cf. Chiles, J.-P. and Delfiner,
P. (1999), p. 92, cf. Gelfand et al. (2010), p. 26).
An important case is $\nu=-0.5$
which gives the covariance function
$$C(r)=\cos(r)$$
and which is only valid for $d=1$. This equals RMdampedcos for $\lambda = 0$, there.
A second important case is $\nu=0.5$ with covariance function
$$C(r)=\sin(r)/r$$ and which is valid for $d \le 3$.
This coincides with RMwave.
Note that all valid continuous stationary isotropic covariance
functions for $d$-dimensional random fields
can be written as scale mixtures of a Bessel type
covariance function with $\nu=\frac{d-2}2$
(cf. Gelfand et al., 2010, pp. 21--22).
References
Chiles, J.-P. and Delfiner, P. (1999)Geostatistics. Modeling Spatial Uncertainty.New York: Wiley.
Gelfand, A. E., Diggle, P., Fuentes, M. and Guttorp,
P. (eds.) (2010)Handbook of Spatial Statistics.Boca Raton: Chapman & Hall/CRL.