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 …

Large wood drives both the form and function of gravel‐bed rivers draining forested basins.
Previously overlooked benefits of wood in rivers are now widely recognized. Together with …

The aim of this work is to investigate how a sequence of anthropic pressures that occurred
on a river sector can generate mutual feedback that determines unplanned channel …

The role of aquatic and riparian vegetation in driving morphodynamics of rivers is being
increasingly recognized across all river types. Here, we focus on gravel‐bed rivers, where …

Abstract Knowledge about historical changes in sediment fluxes in most coarse‐bedded
rivers worldwide is extremely limited. In consideration of this deficiency, we developed a …

Sediment connectivity at the catchment scale includes the processes linking sediment
sources, sinks and the river outlet. Soil erosion models usually estimate yields without …

Summary 450 million people live on river deltas and thus on land that is precariously low
above the sea level and sinking because of human activities and natural processes …

Modeling network‐scale sediment (dis) connectivity and its response to anthropic pressures
provides a baseline understanding of river processes and sediment dynamics that can be …

Free-flowing rivers (FFRs) are fundamental references for river management, providing the
opportunity to investigate river functioning under minimal anthropic disturbance. However …

A variety of stream power‐based approaches for predicting catchment‐scale alluvial
channel adjustment have been developed. There is an international interest in applying …