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 …

Snowfall may have different stable isotopic compositions compared with rainfall, allowing its
contribution to potentially be tracked through the hydrological cycle. This review summarizes …

The interaction of mountain terrain with meteorological processes causes substantial
temporal and spatial variability in snow accumulation and ablation. Processes impacted by …

Owing to drifting snow processes, snow accumulation and surface density in polar
environments are variable in space and time. We present new field data of manual …

Data from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC)
expedition allowed us to investigate the temporal dynamics of snowfall, snow accumulation …

Sea salt aerosols play an important role in the radiation budget and atmospheric
composition over the Arctic, where the climate is rapidly changing. Previous observational …

The wind‐driven saltation of granular material plays a key role in various geophysical
processes on Earth, Mars, Venus, and Titan. Although interparticle cohesion is known to limit …

Preferential deposition of snow and dust over complex terrain is responsible for a wide
range of environmental processes and accounts for a significant source of uncertainty in the …

The surface of the Earth is snow‐covered at least seasonally over large areas. This snow
surface is highly dynamic, particularly under the influence of strong winds. The motion of …

Stable water isotopes from polar ice cores are invaluable high-resolution climate proxy
records. Recent studies have aimed to improve our understanding of how the climate signal …