The geometry of alluvial river channels both controls and adjusts to the flow of water and
sediment within them. This feedback between flow and form modulates flood risk, and the …

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 …

Predicted bedload fluxes often have large errors partly because calculations usually do not
include spatial and temporal flow variability. Sediment motion is driven by a temporal …

To explore the causes of history‐dependent sediment transport in rivers, we use a 19‐year
record of coarse sediment transport from a steep channel in Switzerland. We observe a …

The importance of interactions among stream hydrology, morphology, and biology is well
recognized in studies of stream ecosystems. However, when quantifying the impacts of …

The Swiss plate geophone is a bed load surrogate monitoring system that had been
calibrated in several gravel bed streams through field calibration measurements. Field …

This study focuses on evaluating the sediment mobility and transport patterns in two
Himalayan rivers (Aglar and Paligad Rivers) during monsoon and non‐monsoon flows. The …

The threshold stress for bed sediment transport exerts a primary control on the geometry and
stability of coarse‐grained rivers (diameter≥ 5 mm). Understanding how riverbed mobility …

The influence of boulders in high gradient gravel‐bed rivers can be significant. Yet few
studies have isolated their role in regulating bedload. It is hypothesized that boulder relative …

This study examines the spatial pattern of fractional sediment mobility and assesses the
influence of morphologic units on bedload transport in a small pool‐riffle reach with limited …