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 …

The study of aeolian geomorphological systems over the last half century has advanced
along several important fronts, supported by developments in technologies and analytic …

Wind-driven sand transport generates atmospheric dust, forms dunes, and sculpts
landscapes. However, it remains unclear how the flux of particles in aeolian saltation—the …

Aeolian sediment transport is observed to occur on Mars as well as other extraterrestrial
environments, generating ripples and dunes as on Earth. The search for terrestrial analogs …

The movement of active dunes is tightly linked to climatic conditions (eg, wind regime,
temperature and precipitation) as well as human influence (eg, grazing, dune fixation and …

This paper presents the development, calibration and verification of a fully predictive model
for wind-blown dry sand. The model is based on the modification of the well-known Bagnold …

Emergence and growth of sand dunes results from the dynamic interaction between
topography, wind flow and sediment transport. While feedbacks between these variables are …

This paper reviews the literature on the nature of aeolian creep, the field and wind tunnel
methods used to measure creep transport, the relative contribution of creep transport to total …

Sand patches are one of the precursors to early stage protodunes and occur widely in both
desert and coastal aeolian environments. Here we show field evidence of a mechanism to …

Using particle‐scale simulations of nonsuspended sediment transport for a large range of
Newtonian fluids driving transport, including air and water, we determine the bulk transport …