We present a stochastic modelling of erosion-sedimentation processes. based
on cellular automata, which mimics the natural variability of climatic eve
nts with deterministic transport processes, The numerical procedure calcula
tes the runoff water discharge as a function of the return period of elemen
tary walking elements. This procedure generates water flux distributions at
each point of the system, that depends on the local drainage area. and on
the walker rainfall, and that are statistically analogous to natural river
discharge distributions. It happens that a wide range of non-linear transpo
rt processes can be directly simulated in a intuitive way, relating the wat
er flux and the local slope to the sediment transport activity. The present
version of the code encompasses the main characteristics of erosion-sedime
ntation processes, from the simple hillslope diffusive law to the more comp
lex nonlinear fluvial transport. To illustrate the versatility of the model
to reproduce complex natural dynamics, we calculate several geomorphologic
al instabilities which are crucial in relief dynamics. (C) 2001 Elsevier Sc
ience Ltd. All rights reserved.