We introduce time-dependent boundary conditions in a model of drainage netw
ork evolution based on local erosion rules. The changing boundary condition
s prevent the model from becoming stationary; it approaches a state where f
luctuations of all sizes occur. The fluctuations in the sizes of the draina
ge areas show power law behavior with an exponent that differs significantl
y from that of the static distribution of the drainage areas. Thus, the mod
el exhibits self-organized criticality and proposes a novel concept for pre
dicting fractal properties of drainage networks.