Legacy effects on river sediments are those which alter the location and volume of
sediments and/or presence of contaminants within the sediments as a result of human …

Alteration to the sediment supply of fluvial channels is well understood to trigger
morphological adjustment, but the particularities and peculiarities that arise in any specific …

A substantial increase in fluvial sediment supply relative to transport capacity causes
complex, large-magnitude changes in river and floodplain morphology downstream …

Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …

Abstract Structure-from-Motion (SfM) photogrammetry has become widely used for
topographic data collection in field and laboratory studies. However, the relative …

Recent decades have seen a marked increase in the number of dams removed in the United
States. Investigations following a number of removals are beginning to inform how, and how …

Long‐term prediction of environmental response to natural and anthropogenic disturbances
in a basin becomes highly uncertain using physically based distributed models, particularly …

Additions of sand to gravel beds greatly increase the mobility and flux of gravel. However, it
is not known how additions of finer gravel to coarser gravel beds will affect the mobility of …

Sediment pulses are triggered through a variety of mechanisms, from landslides to land use
change. How do these pulses move through the fluvial system, and how do they evolve? In a …

Sediment transport during flood events often reveals hysteretic patterns because flow
discharge can peak before (counterclockwise hysteresis) or after (clockwise hysteresis) the …