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

Subglacial lakes are repositories of ancient climate conditions, provide habitats for life and
modulate ice flow, basal hydrology, biogeochemical fluxes and geomorphic activity. In this …

Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

The geological record of landforms and sediments produced beneath deglaciating ice
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …

Glacier-erosion rates range across orders of magnitude, and much of this variation cannot
be attributed to basal sliding rates. Subglacial till acts as lubricating 'fault gouge'or 'sawdust' …

Climatic changes over the last 50 years resulted in a decrease of permafrost extent, an
increase of permafrost temperature, and deepening of the active layer in numerous locations …

The temporal variability in sediment export yield from glaciers over a timescale of multiple
glacial cycles (eg 1× 102− 1× 106 years) is of interest for a wide range of applications in …

We identify and map visible traces of subglacial meltwater drainage around the former
Keewatin Ice Divide, Canada, from high-resolution Arctic Digital Elevation Model …

Research on factors affecting sediment regime in glacierized catchments under warming
climates is still scarce despite its societal relevance. In particular, coarse bedload transport …

Lakes are a characteristic feature of glacial landscapes. They are found in the vicinity of
current or past glaciers and ice sheets, in high alpine cirques, inner-alpine valleys as well as …