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 …

Sediments link hillslopes to river channels. The size of sediments entering channels is a key
control on river morphodynamics across a range of scales, from channel response to human …

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 …

Sediment grain size links sediment production, weathering, and fining from fractured
bedrock on hillslopes to river incision and landscape relief. Yet models of sediment grain …

In fluvial networks, some confluences are associated with tributary-driven aggradation
where coarse sediment is stored, downstream sediment connectivity is interrupted and …

Abstract The Dadu River Basin (DRB) is an important economic corridor on the Chuanxi
Plateau. The DRB is located in the highly changeable terrain of the eastern Qinghai-Tibet …

The operation of the Xiaolangdi Reservoir has exerted prominent effects on the processes of
sediment transport and channel evolution in the Lower Yellow River (LYR) since 2000. The …

Sediment supply to rivers, subsequent fluvial transport, and the resulting sediment
connectivity on network scales are often sparsely monitored and subject to major …

Landscape evolution models (LEMs) are an increasingly popular resource for
geomorphologists as they can operate as virtual laboratories where the implications of …

Geomorphic transport laws that describe the movement of material across landscapes
generally hide the role of lithological and climatic boundary conditions behind …