Hydro‐Sedimentological Dynamics in a Compound Bifurcating System of a Large Anabranching River: A Case Study of the Paraná River
Bifurcations in large anabranching rivers are key controls on lateral and longitudinal hydro‐sedimentological connectivity, governing the interactions among flow, sediment transport and channel morphology that drive continuous morphological adjustment and reorganization. Although substantial advances in understanding...