sim_ck(x, data, coords, grid, knn = 12, ordinary = TRUE)multi_tpfit, typically with the output of the function multi_tpfit.NULL all observations are considered (just for very small dataset!!). It is 12 by default.FALSE, the probabilities are computed through the Simple coKriging technique, otherwise the Ordinary coKriging method is used.The probability is calculated as the weighted sum of indicator variables which denote the presence of the $k$-th category in observed points $s_i$. Weights involved in the sum are the solution of a system of equations.
Probabilities approximated are usually truncated and normalized with respect to the probability constraints, because such probabilities might lie outside the interval $[0, 1]$. The normalization procedure is designed such that it is not possible to obtain vectors such that the sum of their probabilities is always equal to one.
When an initial configuration is simulated, it should be modified to reach a pattern similar to the sample by the use of the quench function.
Carle, S. F. (1999) T-PROGS: Transition Probability Geostatistical Software. University of California, Davis.
Sartore, L. (2010) Geostatistical models for 3-D data. M.Phil. thesis, Ca' Foscari University of Venice.
Weise, T. (2009) Global Optimization Algorithms - Theory and Application. http://www.it-weise.de/.
sim_ik, sim_mcs, sim_path