Rivers are important agents of change that shape the Earth's surface and evolve through
time in response to fluctuations in climate and other environmental conditions. They are …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

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 …

The quantification of bedload sediment transport in rivers is possible from statistics of
individual particle displacements. However, there is a lack of empirical basis for a universal …

We review select mature geomorphic transport laws for use in temperate ridge and valley
landscapes and compile parameter estimates for use in applications. This work is motivated …

Many models of incision by bedrock rivers predict water depth and shear stress from
discharge; conversely, palaeoflood discharge is sometimes reconstructed from flow depth …

We present an experimental analysis of hydraulic roughness variations due to changes in
alluvial cover in a mixed bedrock-alluvial meandering channel with larger bedrock …

Assumptions about flow resistance in bedrock channels have to be made for mechanistic
modeling of river incision, paleoflood estimation, flood routing, and river engineering. Field …

Understanding coarse sediment transport is crucial for the prediction of sediment migration
and the consequent development of fluvial morphologies. In this study, cobble …

The critical shear stress (τc) at which grains are entrained on a bedrock surface is important
for determining how bedrock rivers evolve through changes in sediment cover and bedrock …