A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …

Biota are major drivers of geomorphological development. Vegetation and soil fauna act as
ecosystem engineers, changing the environment through physical structures and individual …

Raindrop splashing is one of the driving forces of soil erosion, and it also leads to the loss of
soil nutrients. However, the effects of raindrop splashing on nitrogen loss and the …

Despite considerable community effort, there is no general set of equations to model long‐
term landscape evolution. In order to determine a suitable set of landscape evolution …

Climate change is causing increasingly widespread, frequent, and intense wildfires across
the western United States. Many geomorphic effects of wildfire are relatively well studied, yet …

Hillslopes constitute the majority of a drainage basin space, and they, together with
channelized streams and mountain glaciations, form the most representative exogenic …

Recent studies have emphasized the importance of nonlocal models in characterizing
bedload transport in natural rivers, particularly in mixed-size gravel beds or steep hillslopes …

Wind‐driven tree throw is an observable and consequential process that suddenly moves
soil downslope, inverts the soil column, and roughens the surface with pit‐mound …

Models of landscape evolution provide insight into the geomorphic history of specific field
areas, create testable predictions of landform development, demonstrate the consequences …

Assessing rivers' and hillslopes' sensitivity to external forcing is paramount to understand
landscape evolution, in particular as a response to Quaternary climate changes. River …