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 …

One of the pillars of geomorphology is the study of geomorphic processes and their drivers,
dynamics, and impacts. Like all activity that transfers energy to Earth's surface, a wide range …

The temporal variability in sediment export yield from glaciers over a timescale of multiple
glacial cycles (eg 1× 102− 1× 106 years) is of interest for a wide range of applications in …

Bedload transport drives morphological changes in gravel‐bed streams and sediment
transfer in catchments. The large impact forces associated with bedload motion and its …

Measuring bedload transport rates usually involves measuring the flux of sediment or
collecting sediment during a certain interval of time Δ t. Because bedload transport rates …

About 10% of Europe's surface area is prone to rapid flooding of rivers confined in valleys.
The devastating potential of such floods is exacerbated by the deficits of existing gauging …

The Swiss plate geophone is a bedload surrogate monitoring system that has been
calibrated in several gravel‐bed streams using direct sampling techniques. Past systematic …

Alpine glaciers are rapidly retreating due to global warming and this has been associated
with enhanced supply of subglacially derived sediment to downstream environments. We …

Understanding and predicting bedload transport is an important element of watershed
management. Yet, predictions of bedload remain uncertain by up to several order (s) of …

Bedload transport is a key process in fluvial morphodynamics, but difficult to measure. The
advent of seismic monitoring techniques has provided an alternative to in‐stream …