Resistance to flow determines several important hydraulic parameters in streams and rivers
and must be properly represented in models for estimating water discharge and sediment …

An uncertainty analysis of the unsteady flow component (UNET) of the one-dimensional
model HEC-RAS within the generalised likelihood uncertainty estimation (GLUE) is …

A data set of 2890 field measurements was used to test the ability of several conventional
flow resistance equations to predict mean flow velocity in gravel bed rivers when used with …

Alternative general forms are considered for equations to predict mean velocity over the full
range of relative submergence experienced in gravel‐and boulder‐bed streams. A partial …

Steep, rough channels occupy a large fraction of the total channel length in mountainous
regions. Most sediment mobilized on hillslopes must pass through these streams before …

The present study examines variations in the reference shear stress for bed load transport
(τr) using coupled measurements of flow and bed load transport in 45 gravel‐bed streams …

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 …

Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 19. What are the forms and processes characteristic of mountain rivers and …

Fluvial Hydraulics provides a sound qualitative and quantitative understanding of water and
sediment flows in natural rivers. This understanding is essential for modeling and predicting …

We measured velocity and channel geometry in 10 reaches (bed gradient= 0.08–0.21) of a
predominantly step-pool channel, the Rio Cordon, Italy, over a range of discharges (3–80 …