The ability to model surface processes and to couple them to both subsurface and
atmospheric regimes has proven invaluable to research in the Earth and planetary sciences …

Abstract The Mountain Front Flexure marks a dominant topographic step in the frontal part of
the Zagros Fold–Thrust Belt. It is characterized by numerous active anticlines atop of a …

Representation of flowing water in landscape evolution models (LEMs) is often simplified
compared to hydrodynamic models, as LEMs make assumptions reducing physical …

Models of landscape evolution by river erosion are often either transport-limited (sediment is
always available but may or may not be transportable) or detachment-limited (sediment must …

Paleoearthquake studies that inform seismic hazard rely on assumptions of sediment
transport that remain largely untested. Here, we test a widespread conceptual model and a …

We develop a hydroclimatological approach to the modeling of regional shallow landslide
initiation that integrates spatial and temporal dimensions of parameter uncertainty to …

We consider deterministic and probabilistic cellular automata to study and describe certain
types of patterns in idealized material blocks. We have particular interest in patterns similar …

Facets formed along the footwalls of active normal‐fault blocks display a variety of
longitudinal profile forms, with variations in gradient, shape, degree of soil cover, and …

A new particle-based reduced-complexity model to simulate sediment transport and channel
morphology in steep streams in presented. The model CAST (Cellular Automaton Sediment …

This paper describes and explores a new continuous-time stochastic cellular automaton
model of hillslope evolution. The Grain Hill model provides a computational framework with …