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

Earth's climate is warming and will continue to warm as the century progresses. High
mountains and high latitudes are experiencing the greatest warming of all regions on Earth …

Climate change impacts on sediment production and transfer processes on hillslopes and
through channels are governed by possible changes in precipitation, runoff, and air …

In recent decades, slope instability in high‐mountain regions has often been linked to
increase in temperature and the associated permafrost degradation and/or the increase in …

Controlling sediment to reduce debris-flow hazard is generally approached using retention
basins that can be closed or have an outlet structure, generally an open check dam. They …

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 …

In the European Alps almost half the glacier volume disappeared over the past 150 years.
The loss is reflected in glacier retreat and ice surface lowering even at high altitude. In steep …

Just as glaciers worldwide left a record of past advances and retreats that shifted latitudinally
in response to oscillating Quaternary climate changes, so too have cold-climate conditions …

This study exploited the historical rockfall inventory and the meteorological stations
database of Mont Cervin and Mont Emilius Mountain Communities (Aosta Valley, northern …

Mountainous topography reflects an interplay between tectonic uplift, crustal strength, and
climate-conditioned erosion cycles. During glaciations, glacial erosion increases bedrock …