Predicting the morphodynamics of sedimentary landscapes due to fluvial and aeolian flows
requires answering the following questions: Is the flow strong enough to initiate sediment …

Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …

Rivers are important agents of change that shape the Earth's surface and evolve through
time in response to fluctuations in climate and other environmental conditions. They are …

The geometry of alluvial river channels both controls and adjusts to the flow of water and
sediment within them. This feedback between flow and form modulates flood risk, and the …

Earth's surface is composed of a staggering diversity of particulate–fluid mixtures: dry to wet,
dilute to dense, colloidal to granular and attractive to repulsive particles. This material variety …

I describe a configurable machine‐learning framework to estimate a suite of continuous and
categorical sedimentological properties from photographic imagery of sediment, and to …

Vegetation provides habitat and nature‐based solutions to coastal flooding and erosion,
drawing significant interest in its restoration, which requires an understanding of sediment …

While the influence of large grains on the morphodynamics of gravel‐bed rivers has long
been recognized, nothing dominates our collective efforts to model such rivers like the bed …

Understanding river response to sediment pulses is a fundamental problem in geomorphic
process studies, with myriad implications for river management. However, because large …

Predicted bedload fluxes often have large errors partly because calculations usually do not
include spatial and temporal flow variability. Sediment motion is driven by a temporal …