Earth's terrestrial topography evolves in response to the interaction of tectonics, climate, and
lithology. Recent discoveries suggest that the grain size of sediments produced on hillslopes …

A major control on bedrock incision is the interaction between alluvial cover and erosive
mobile grains. The extent of alluvial cover is typically predicted as a function of relative …

Understanding the physical processes driving bedrock channel formation is essential for
interpreting and predicting the evolution of mountain landscapes. Here we analyze bedrock …

Tectonically active mountain regions such as Southwestern China are frequently hit by
catastrophic floods caused by the breach of landslide dams. However, how these extreme …

Results from computational morphodynamics modeling of coupled flow–bed–sediment
systems are described for 10 applications as a review of recent advances in the field. Each …

Bedrock channel slope and width are important parameters for setting bedload transport
capacity and for stream-profile inversion to obtain tectonics information. Channel width and …

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 …

Sediment yields from glacierized basins are used to quantify erosion rates on seasonal to
decadal timescales as well as conditions at the glacier bed, and eskers hold valuable …

Erosional perturbations from changes in climate or tectonics are recorded in the profiles of
bedrock rivers, but these signals can be challenging to unravel in settings with non‐uniform …

Geomorphologists often rely on simple models of river channel incision for predicting rates
of landscape evolution and channel response to perturbations, as well as extracting climatic …