Bifurcations are important geomorphological features in tide‐influenced deltas. At
bifurcations, river flow and tides distribute sediment over the channel network and determine …

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 …

Free alternate bars are large‐scale, downstream‐migrating bedforms characterized by an
alternating sequence of three‐dimensional depositional fronts and scour holes that …

Looping patterns, where channels divide and reconnect further downstream, are
widespread in natural rivers. Here, we build an extensive dataset of different gravel‐bed and …

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 striking feature of rivers is their ability to sort the sediments composing them. One of the
chief causes for grain sorting consists in the selective transport of different sizes moving …

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 …

Deltaic channel networks are important conduits for water and material supplies to the fluvial
and coastal communities. However, increasing human interventions in river deltas have …

Confluences act as crucial intersection in a fluvial system as they regulate the flow,
sediment, and geomorphological stability. Two of the natural occurrences that have an effect …