Abstract Low-gradient fluvial landscapes (1–50 cm km− 1) occupy diverse settings (inland,
tidal, and deltaic wetlands, large-river floodplains, lowland streams) but share many …

Meandering planforms are common on rivers but active, rapidly changing meandering
channels are particularly instructive in indicating meander processes and dynamics and can …

Dynamic interaction between river morphodynamics and vegetation affects river channel
patterns and populations of riparian species. A range of numerical models exists to …

The morphological development of fluvial and tidal systems is forecast more and more
frequently by models in scientific and engineering studies for decision making regarding …

River morphology and riparian vegetation continuously adapt to changing discharge
conditions, which makes it a challenge to distinguish long-term development driven by …

Accurate records of flash flood magnitudes are required to inform flood forecasting and
planning. However, whilst a distributed flood survey is desirable to capture spatial …

Cohesive floodplain sediment and vegetation are both thought to cause meandering river
patterns. Our aims are to compare the isolated and combined effects of mud and vegetation …

River meandering results from spatially alternating bank erosion and bar growth. Recent
flume experiments and theory suggest that a continuous inflow perturbation is a requirement …

Recent studies suggest that braided river could be single-thread channel by colonization of
riparian vegetation; however, this kind of mutual interactions between physical and …

Channel bifurcations control the distribution of water and sediment in deltas, and the routing
of these materials facilitates land building in coastal regions. Yet few practical methods exist …