The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …

Recent advances in our understanding of estuarine circulation and salinity structure are
reviewed. We focus on well-and partially mixed systems that are long relative to the tidal …

Rivers and Floodplains is concerned with the origin, geometry, water flow, sediment
transport, erosion and deposition associated with modern alluvial rivers and floodplains …

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 …

In a channel with bed topography that does not vary in the downstream direction, a
secondary circulation composed of outward flow at the surface and inward flow near the …

Meandering rivers are diagnostic landforms of hydrologically active planets, and their
migration regulates the continental component of biogeochemical cycles that stabilize …

Bed load transport in Muddy Creek, Wyoming, a sand‐bedded meandering river with
equilibrium bottom topography, was found to consist of a zone of maximum sediment flux …

Measurements of downstream and cross-stream velocities at a small, asymmetrical stream
confluence show that the structure of low-stage flows is influenced by the tributary/main stem …

The boundary shear stress pattern and the superelevation of the water surface in a meander
on a small stream are predicted from two simple equations representing a frictionally …

The migration rate of sharp meander bends exhibits large variance and indicates that some
sharply curved bends tend to stabilize. These observations remain unexplained. This paper …