A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …

Stream hydromorphology regulates in‐stream water flow and interstitial flow of water within
streambed sediments, the latter known as hyporheic exchange. Whereas hyporheic flow has …

Large particles strongly influence flow resistance, energy dissipation, bed stability, and
channel morphology in mountain streams. We conducted flume experiments to evaluate …

High resolution topographic data are necessary to understand benthic habitat, quantify
processes at the water-sediment interface, and support computational fluid dynamics …

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 …

Salmonids create an egg nest, called a redd, in hyporheic streambed gravel to bury their
eggs, characterized by a pit and a hump topography, resembling a dune. Embryos' survival …

A common approach used to mitigate riverbank erosion and maintain watercourse
alignments has been through the application of riprap or larger, more stable particles to …

In northern Fennoscandia, semi‐alluvial boulder‐bed channels with coarse glacial legacy
sediment are abundant, and due to widespread anthropogenic manipulation during timber …

Topographic variation within fluvial systems is essential for providing a mosaic of physical
habitats and supporting the dynamic hydraulic, geochemical, and biological processes that …

In this paper, the results of numerical simulations of open-channel flow through boulder
arrays at varying Froude numbers are reported. The simulations aim at clarifying the role of …