Sep 2026
Modeling dynamic equilibrium in a braided river using a fully coupled two-dimensional hydro-morphodynamics framework
Sediment transport governs the dynamic exchange of sediment and flow that underpins channel–floodplain interactions and is a primary controller of fluvial morphology in large alluvial braided rivers. Quantitative analysis of sediment flux is essential to determine whether the river bed is in a dynamic equilibrium or...
Rohan Choudhury, Anurag Handique, A. Baruah et al.
· Water Practice & Technol... · 0 citations