The rate of river migration affects the stability of Arctic infrastructure and communities, and
regulates the fluxes of carbon,, nutrients and sediment, to the oceans. However, predicting …

Most ways of predicting flow resistance in shallow rivers with a partial or complete cover of
coarse sediment use a bed‐sediment grain diameter as a roughness length scale. However …

Bedrock incision plays a key role in determining the pace of landscape evolution. Much is
known about how bedrock rivers incise vertically, but less is known about lateral erosion …

Bed roughness height (k) is a key parameter for velocity prediction in open‐channel flows.
There is not yet a firm consensus about whether characteristic particle size D84 or (standard …

In natural and restored rivers, protruding river‐bed elements can cause complex flow
patterns. We hypothesize that, particularly at very low flows, solute spreading in such …

A parameterized expression for sand wave morphology in rivers is established using a flow
resistance law while accounting for sediment incipient velocity. A distinct relation is drawn …

Macro-roughness elements such as boulders and bedrock outcrops, collectively referred to
as large bed elements (LBEs), are key features influencing hydrodynamics and …

Uncertainty analysis of hydrological models often requires a large number of model runs,
which can be time consuming and computationally intensive. In order to reduce the number …

We present an experimental analysis of hydraulic roughness variations due to changes in
alluvial cover in a mixed bedrock-alluvial meandering channel with larger bedrock …

Several studies have demonstrated the importance of alluvial cover; furthermore, several
mathematical models have also been introduced to predict the alluvial cover on bedrock …