The Cantor dust model for discontinuity in geomorphic process rates
The temporal discontinuity in geomorphic processes that is responsible for time-scale dependence in published process rates (Gardner et al., 1987) is effectively modeled by a fractal construction, the Cantor dust. Fractal dimension values estimated
This study examines the usefulness of the Cantor dust as a method to characterize precipitation records from climate stations in the arid/semiarid zone of the Southwestern United States. Because many geomorphic processes dependent on precipitation