The temporal evolution of seasonal snow cover and its spatial variability in environments
such as mountains, prairies or polar regions is strongly influenced by the interactions …

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 …

This publication presents a comprehensive hydrometeorological data set for three research
sites in the upper Rofental (1891–3772 m asl, Ötztal Alps, Austria) and is a companion …

Wind-blown snow is a frequent phenomenon in high-elevation and polar regions which
impacts the surface energy and mass balance of these areas. Loose surface snow gets …

To date, most studies on coupled-water-and-heat processes in frozen soils haves focused
on the mechanism of changes in frozen soil and the contribution of climate change …

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 …

The surface of Antarctica is continuously shaped by erosion, blowing snow and deposition,
resulting in diverse aeolian bedforms akin to those observed in subtropical sand deserts …

Wind-induced snow transport has a strong influence on snow spatial variability especially at
spatial scales between 1 and 500 m in alpine environments. Thus, the evolution of snow …

Air and near-surface ground temperatures were measured using dataloggers over 14 years
(2006–2020) in 10 locations at 2262 to 2471 masl in a glacial cirque of the Cantabrian …

Drifting snow is a significant factor in snow redistribution and cascading snow incidents.
However, field observations of drifting snow are relatively difficult due to limitations in …