Self-organized critical drainage networks.
We introduce time-dependent boundary conditions in a model of drainage network evolution based on local erosion rules. The changing boundary conditions prevent the model from becoming stationary; it approaches a state where fluctuations of all sizes occur. The fluctuations in the sizes of the drainage areas show power law behavior with an exponent that differs significantly from that of the static distribution of the drainage areas. Thus, the model exhibits self-organized criticality and proposes a novel concept for predicting fractal properties of drainage networks.
Hergarten
S
S
Geodynamics-Physics of the Lithosphere, University of Bonn, Bonn, Germany. hergarten@geo.uni-bonn.de
Neugebauer
H J
HJ