Process-product studies have been central to the development of process sedimentology
over the past few decades, with the ability to first measure flows, and then examine the …

Strong feedbacks exist between channel dynamics, floodplain development, and riparian
vegetation. Earlier experimental studies showed how uniformly distributed riparian …

Remotely sensed imagery of rivers has long served as a means for characterizing channel
properties and detection of planview change. In the last decade the dramatic increase in the …

Abstract The Three Gorges Dam (TGD) has altered downstream flow–sediment regimes and
led to significant changes in the morphodynamic processes in the Middle Yangtze River …

Although it has long been recognized that deposition along meandering rivers is not
restricted to convex banks (ie, point bars), the consensus is that sediment deposition on …

Community coalescence, ie, the mixing and merging of microbial communities and their
surrounding environments, is prevalent in various ecosystems and potentially acts on …

It remains an open question how the hydrodynamics and morphology in sharp meander
bends adapt to the changes in flow and sediment conditions induced by upstream damming …

Despite being a primarily depositional landform, a crevasse splay experiences an initial
evolutionary phase that is primarily erosional as sediment-laden river water spills from a …

The three‐dimensional flow field near the banks of alluvial channels is the primary factor
controlling rates of bank erosion. Although submerged slump blocks and associated large …

Compound meander bends with multiple lobes of maximum curvature are common in
actively evolving lowland rivers. Interaction among spatial patterns of mean flow, turbulence …