Key points are not available for this paper at this time.
Geostatistical simulations often require the generation of numerous realizations of a stationary Gaussian process over a regularly meshed sample grid. This paper shows that for many important correlation functions in geostatistics, realizations of the associated process over m+1 equispaced points on a line can be produced at the cost of an initial FFT of length 2m with each new realization requiring an additional FFT of the same length. In particular, the paper first notes that if an (m+1) (m+1) Toeplitz correlation matrix R can be embedded in a nonnegative definite 2M2M circulant matrix S, exact realizations of the normal multivariate y N (0, R) can be generated via FFTs of length 2M. Theoretical results are then presented to demonstrate that for many commonly used correlation structures the minimal embedding in which M = m is nonnegative definite. Extensions to simulations of stationary fields in higher dimensions are also provided and illustrated.
Dietrich et al. (Tue,) studied this question.