Plants growing within river corridors both affect and respond to fluvial processes. Their
above‐ground biomass modifies the flow field and retains sediment, whereas their below …

Salt marshes are dynamic systems able to laterally expand, contract, and vertically accrete
in response to sea level rise. Here, we present the grand challenges that need to be …

This paper highlights some recent trends in vegetation hydrodynamics, focusing on
conditions within channels and spanning spatial scales from individual blades, to canopies …

The presence of vegetation modifies flow and sediment transport in alluvial channels and
hence the morphological evolution of river systems. Plants increase the local roughness …

More than half of the original Everglades extent formed a patterned peat mosaic of elevated
ridges, lower and more open sloughs, and tree islands aligned parallel to the dominant flow …

Despite the rapid construction of offshore wind farms, the available information regarding the
risks of this type of development in terms of emerging pollutants, particularly microplastics, is …

Quantifying hydrologic and ecological connectivity has contributed to understanding
transport and dispersal processes and assessing ecosystem degradation or restoration …

Mechanisms reported to promote landscape self-organization cannot explain vegetation
patterning oriented parallel to flow. Recent catastrophic shifts in Everglades landscape …

The structure of the bottom boundary layer (BBL) in aquatic flows influences a range of
biophysical processes, including sediment transport, hyporheic exchange, and biofilm …

Vegetation is a common feature in natural coastal and riverine water ways, interacting with
both the water flow and sediment transport. However, the physical processes governing …