The morphology of an alluvial river channel is the consequence of sediment transport and
sedimentation in the river. Morphological style is determined chiefly by the caliber and …

Proglacial systems are amongst the most rapidly changing landscapes on Earth, as glacier
mass loss, permafrost degradation and more episodes of intense rainfall progress with …

Abstract System-scale detection of erosion and deposition is crucial in order to assess the
transferability of findings from scaled laboratory and small field studies to larger spatial …

The estimation of fluvial sediment transport rate from measurements of morphological
change has received growing recent interest. The revival of the 'morphological …

Accurate characterisation of morphology is critical to many studies in the field of
geomorphology, particularly those dealing with changes over time. Digital elevation models …

Previous studies of channel morphological change have often relied upon sparse spatial
and temporal data-sets, resulting in a degree of uncertainty in their conclusions …

A key aspect of geomorphological enquiry is concerned with quantitatively monitoring the
development of the Earth's surface, in a diverse set of environments, and at a range of …

Quantifying the morphology of braided rivers is a key task for understanding braided river
behaviour. In the last decade, developments in geomatics technologies and associated data …

This paper compares two approaches used to derive measures of annual sediment transfers
within a 1 km long piedmont reach of the gravel-bed River Coquet in Northumberland …

Three-dimensional morphological adjustment in a chute cutoff (breach) alluvial channel is
quantified using Digital Elevation Model (DEM) analysis for a ca. 0.7 km reach of the River …