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

Understanding climatic influences on the rates and mechanisms of landscape erosion is an
unresolved problem in Earth science that is important for quantifying soil formation rates …

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 …

In mountainous landscapes the role of periglacial processes in producing sediment is poorly
defined, despite evidence of abundant talus slopes. Ice growth in rock has long been …

The intensification of thaw-driven mass wasting is transforming glacially conditioned
permafrost terrain, coupling slopes with aquatic systems, and triggering a cascade of …

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

Diverse field data on glacial sediment yields are assembled in the context of the current
interest in sedimentary basin development in glaciated regions, and in controversial …

Quantitative estimates of sediment flux and the global cycling of sediments from hillslopes to
rivers, estuaries, deltas, continental shelves, and deep-sea basins have a long research …

This review article deals with bank erosion from the perspective of rivers affected by
seasonal ice formation. These rivers drain half of the terrestrial land surface globally, and …

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 …