Alteration to the sediment supply of fluvial channels is well understood to trigger
morphological adjustment, but the particularities and peculiarities that arise in any specific …

Over the last decade several computational models, and several types of model, have been
developed to simulate the response of river systems to environmental change over time …

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 …

Like many rivers in the western US, the Elwha River, Washington, has changed substantially
over the past century in response to natural and human forcing. The lower river is affected by …

Most studies investigating fine sediment ingress in gravel-bed rivers have been conducted
at the laboratory scale, and even fewer have explored the ingress processes of flocculated …

An expert-based approach was used to identify 10 morphological unit types within a reach of
the gravel bed, regulated Yuba River, California, that is heavily utilized by spawning …

Resource managers, scientists, government regulators, and stakeholders are considering
sophisticated numerical models for managing complex environmental problems. In this …

Historical range of variability (HRV) describes the range of temporal and spatial variations in
river variables such as flow regime or channel planform prior to intensive human alteration …

In this paper, we present a methodology to construct a sediment budget for meso‐scale
catchments. We combine extensive field surveys and expert knowledge of the catchment …

The relationships between flow hydrology, topography, and channel change in mountain
rivers is important to understanding landscape evolution, the structure and persistence of …