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

In glacier forefields, the chronosequence approach is used to investigate ecological,
biogeochemical and physical features of autogenic successional change as a function of …

Accelerated glacier and ice sheet retreat and thinning in recent decades has profound
consequences for catchment sediment supply with attendant repercussions for nutrient …

Glacial lake outburst floods (GLOFs) are a major natural hazard in high mountain regions
and have caused significant loss and damage. In the past decade, two lakes (Ranzeria Co …

In the past decade, sediment connectivity has become a widely recognized characteristic of
a geomorphic system. However, the quantification of functional connectivity (ie connectivity …

The combined analysis of past evolutionary trajectories of channel morphology and
temporal patterns of driving factors is fundamental to understanding present river conditions …

In mountain rivers, long‐term observations of water and sediment fluxes are crucial for
understanding the dynamics of bedload fluctuations. We analyze 7 years of continuous data …

ABSTRACT High-Resolution Topography (HRT) data sets are becoming increasingly
available, improving our ability and opportunities to monitor geomorphic changes through …

Proglacial areas in high-mountain environments are among the most dynamic landscape
zones in terms of morphological, sedimentological, and hydrological changes. In fact, in …

Alpine glaciers are rapidly retreating due to global warming and this has been associated
with enhanced supply of subglacially derived sediment to downstream environments. We …