Dry rivers are a type of non-perennial river characterized by extreme dry conditions and
dominance of terrestrial habitats. They are present in all continents, being especially …

We define Dry Rivers as those whose usual habitat in space and time are dry channels
where surface water may interrupt dry conditions for hours or a few days, primarily after …

River beds are often arranged into patches of similar grain size and sorting. Patches can be
distinguished into “free patches,” which are zones of sorted material that move freely, such …

Steep streams occupy a large fraction of mountainous drainage basins and partially control
the sediment supplied to downstream rivers. In these channels, sediment transport …

In mountainous drainage networks, sediment mobilized on hillslopes must first pass through
steep streams before reaching lower‐gradient channels. The bed of steep channels is …

A system has been installed to automatically monitor rainfall, streamflow, bedload discharge
and suspended sediment concentration in the arid to hyper‐arid setting of Nahal Rahaf …

River beds are traditionally assumed to become mobile at a fixed value of nondimensional
shear stress, but several flume and field studies have found that the critical value is higher in …

This paper provides novel observations linking the connections between spatially distributed
bed load transport pathways, hydraulic patterns, and morphological change in a shallow …

An automatic bedload monitoring station has been established on the perennial Tordera
River, a Mediterranean mountain gravel-bed stream located in NE Spain. Bedload fluxes …

Bed load discharge formulas have been evaluated by analyzing them in relation to
measured Helley–Smith data for the gravel-bedded armored Drau River, Austria …