One‐dimensional models for river bifurcations rely on a nodal point relation that determines
the distribution of sediments between the downstream branches. The most widely‐adopted …

The Earth's landscape hosts a variety of patterns resulting from the interaction between a
sediment-carrying fluid and an erodible boundary. Here, the morphodynamics of river …

A diffluence-confluence unit on a meandering channel, coupled with the broadening of the
divergence zone and meander circulation, promotes sediment deposition on the convex …

The evolution of fluvial systems is greatly impacted by mid-channel bars, a typical
morphodynamic process in natural rivers. Sometimes, the growth of vegetation over these …

Channel bifurcations are common features observed in fluvial landforms from upstream
gravel‐bed rivers to downstream deltas. Extensive research has been carried out to study …