G Seminara - Annual Review of Fluid Mechanics, 2010 - annualreviews.org
Geomorphology is concerned with the shaping of Earth's surface. A major contributing mechanism is the interaction of natural fluids with the erodible surface of Earth, which is …
G Seminara - Journal of fluid mechanics, 2006 - cambridge.org
In the last few decades cooperation among fluid dynamicists and geomorphologists has allowed the construction of a rational framework for the quantitative understanding of several …
JM Hooke - Treatise on geomorphology, 2013 - researchgate.net
Various phases of progress and differing approaches to research on river meandering are identified. Since early quantification of equilibrium relations of meander morphology to …
D Termini, M Piraino - Earth Surface Processes and Landforms, 2011 - Wiley Online Library
Flow in meandering bends is characterized by the formation of a large cross‐sectional central‐region circulation cell. The width‐to‐depth ratio is one of the most important …
G Zolezzi, R Luchi, M Tubino - Reviews of Geophysics, 2012 - Wiley Online Library
Most morphodynamic models of river meandering assume spatially constant width; depending on the intensity of spatial width variations, different meandering styles actually …
W Bertoldi, M Tubino - Water Resources Research, 2007 - Wiley Online Library
In this work we have investigated the equilibrium configurations of a Y‐shaped fluvial bifurcation through a laboratory analysis. Three series of experimental runs have been …
L Adami, W Bertoldi, G Zolezzi - Water Resources Research, 2016 - Wiley Online Library
We report on a multidecadal analysis of alternate bar dynamics in a 41.7 km reach of the Alpine Rhine River, which represents an almost unique example of a regulated river with …
We study the numerical approximation of the two-dimensional morphodynamic model governed by the shallow water and Exner equations to simulate reach-scale two …
S Lanzoni, G Seminara - Journal of Geophysical Research …, 2006 - Wiley Online Library
Bend instability is the process whereby perturbations of the planform distribution of a channel relative to a straight configuration may grow, driven by erosion at concave banks …