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 …

Most ways of predicting flow resistance in shallow rivers with a partial or complete cover of
coarse sediment use a bed‐sediment grain diameter as a roughness length scale. However …

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 …

Abstract The Surface Water and Ocean Topography Mission (SWOT) will generate global,
spatially continuous maps of water surface elevation and extent for large inland water …

The transferability of hydraulic microhabitat selection models among rivers has been largely
debated. It can influence management decisions such as restoration measures or …

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 …

A 524‐km reach of Fraser River, British Columbia, was traversed, where the channel
alternates between gravel‐bedded reaches that are incised into semiconsolidated glacial …

This study initially examines the various sources of flow resistance in sand-bed (lowland)
and gravel-bed (mountainous) rivers along with the limitations of traditional estimation …

Pollution abatement and flood control activities require effective water resource planning,
engineering assessment, sophisticated technology, and appropriate hydraulic structure …