The grain‐scale morphology of fluvial sediments is an important control on the character and dynamics of river systems; however current understanding of its role is limited by the …
Repeat topographic surveys are often used to monitor geomorphological change in rivers. Such surveys can yield Digital elevation models (OEMs), which are differenced against each …
The progressive degradation of the cryosphere of High-Arctic areas causes an increase in the dynamics of geomorphic processes that shape the valleys of rapidly retreating glaciers …
The article presents calculations of quantitative modifications of the morphology of selected subsystems of a glacial valley through:(i) identification of the spatial distribution of important …
Numerical models that predict channel evolution are an essential tool for investigating processes that occur over timescales which render field observation intractable. The current …
Morphological change in gravelly river channels and active slope environments can be used to derive lower-bound estimates of sediment flux between successive dates on which the …
Numerical models that predict channel evolution through time are an essential tool for investigating processes that occur over timescales which render field observation …
This study investigates sediment transport processes and sediment-landform development at two small valley glaciers of contrasting basal thermal-regime. A range of innovative …