A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …

River widening, defined as a lateral expansion of the channel, is a critical process that
maintains fluvial ecosystems and is part of the regular functioning of rivers. However, in …

The evolution of rivers in eroding landscapes plays a key role in determining landscape
relief and modulating climate‐tectonic interactions. A common approach to quantifying river …

Sediment supply (Qs) is often overlooked in modelling studies of landscape evolution,
despite sediment playing a key role in the physical processes that drive erosion and …

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 …

River management is founded on predictable self‐organisation between river form and
catchment controls in alluvial rivers. However, a substantial proportion of rivers are not fully …

The structural controls of sediment connectivity are poorly understood in low-gradient
watersheds and stream networks. We developed a field-and modeling-based framework to …

Abstract Analysis of hillslope gradient, landscape relief, and channel steepness in the Daxia
River basin provides evidence of a transient geomorphic response to base‐level fall on the …

Rivers are dynamical systems that are thought to evolve towards a steady-state
configuration. Then, geomorphic parameters, such as channel width and slope, are constant …

Landscape evolution is a product of the forces that drive geomorphic processes (eg,
tectonics and climate) and the resistance to those processes. The underlying lithology and …