The distinction often made between active and passive restoration approaches is a false
dichotomy that persists in much research, policy, and financial structures today. We explore …

Riparian zones are dynamic ecosystems that form at the interface between the aquatic and
terrestrial components of a landscape. They are shaped by complex interactions between …

We propose a conceptual model of vegetation–hydrogeomorphology interactions and
feedbacks within river corridors (ie river channels and their floodplains) that builds on …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

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 …

Logjams create diverse physical and ecological effects in stream channels, including at least
temporary storage of water, sediment, and particulate organic matter. We hypothesize that …

Africa's population is expected to triple by 2050, owing to rapid urbanisation and overall
demographic trends. The combined pressures of urbanisation and climate change impact …

Rivers are dynamic landscape features that change in response to natural and
anthropogenic factors through hydrological, geomorphic and ecological processes. The …

Gravel-bed rivers are fluvial systems featuring highly complex morphological and
evolutionary patterns because of their configuration characterized by the contemporary …

A set of multi-scale, process-based hydromorphological indicators of river character and
dynamics has been developed to support river management and restoration activities …