River dams provide many benefits, including flood control. However, due to constantly
evolving channel morphology, downstream conveyance of floodwaters following dam …

The bed of fluvial ecosystems plays a major role in global biogeochemical cycles. All fluvial
sediments migrate and although responses of aquatic organisms to such movements have …

River dunes are wavelike features in sandy riverbeds that move slowly in a downstream
direction. These bedforms are shaped by the interaction between flowing water and sand …

Large‐scale wave flume experiments are conducted in the ripple vortex regime to study near
bed coarse sand transport processes below asymmetric surface waves typical of the coastal …

River dunes, dynamic bedforms in the river bed, limit navigable depths during low flows and
increase bed roughness. To predict the navigable depth or where maintenance dredging is …

Dune dimensions in sand‐bedded rivers are often thought to scale with flow depth (h), with
height (H) scaling as 1/6h and length (L) as 5h, even though substantial scatter about the …

Fluvial instabilities originate from an interplay between the carrier fluid and the erodible
loose boundary at their interface, manifesting a variety of sedimentary architectures with …

Fluvial cross strata are depositional products of bedform migration that record formative flow
and sediment transport conditions on planetary bodies. Bedform evolution varies with …

Flow separation behind the dune forms may have reduced the contact area between the
flows and the bed surface, in addition to producing form drag in open channels. In this study …