Rapid atmospheric warming since the mid-twentieth century has increased temperature-
dependent erosion and sediment-transport processes in cold environments, affecting food …

Proglacial areas represent the counterpart of glacial retreat, where a new environmental
equilibrium will be reached. During this long and complex stage, which represents the …

Global warming promotes glacier retreat, snow melting, and permafrost thawing, thereby
increasing landslide activity in alpine mountain regions. However, our understanding of the …

Climate change affects cryosphere-fed rivers and alters seasonal sediment dynamics,
affecting cyclical fluvial material supply and year-round water-food-energy provisions to …

Alps are an important geographical area of the European continent and, in this area,
temperature increase is most evident. However, the 1991–2020 climate normal in the Alps …

We describe and model the evolution of a recent landslide, tsunami, outburst flood, and
sediment plume in the southern Coast Mountains, British Columbia, Canada. On November …

Ongoing global warming intensifies the degradation of permafrost. Permafrost thawing
impacts landform evolution, reduces freshwater resources, enhances the potential of natural …

Rockfall in high-mountain regions is thought to be changing due to accelerating climate
warming and permafrost degradation, possibly resulting in enhanced activity and larger …

The massive worldwide deglaciation leads to more frequent slope instabilities in
mountainous terrains. The physical processes leading to such destabilizations are poorly …

High-magnitude mass flows can have a pervasive geomorphological legacy, yet the short-
term response of valley floors to such intense disturbances is poorly known and poses …