We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …

Glacier change is ubiquitous, but the fastest and largest magnitude changes occur in
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …

We used Little Ice Age (LIA) trimlines and moraines to assess changes in South American
glaciers over the last~ 140 years. We determined the extent and length of 640 glaciers …

The contribution to sea level rise from Patagonian icefields is one of the largest mass losses
outside the large ice sheets of Antarctica and Greenland. However, only a few studies have …

The northern and southern Patagonian ice fields (NPI and SPI) have been subject to
accelerated retreat during the last decades, with considerable variability in magnitude and …

The complex dynamics of calving glaciers is a major uncertainty in projecting global glacial
mass loss. We present frontal ablation and ice mass change for the 38 major calving …

Patagonian icefields are losing volume, and their loss is due partly to rapid changes in their
outlet glaciers that terminate in lakes or the ocean. Despite this key influence from outlet …

Glacier and permafrost hazards such as glacial‐lake outburst floods and rock–ice
avalanches cause significant socio‐economic damages worldwide, and these processes …

We present the first comprehensive high‐resolution mosaic of ice velocity of the Northern
(NPI) and Southern Patagonian Icefields (SPI), from multiple synthetic aperture radar and …

We present surface mass balance simulations of the Southern Patagonia Icefield (SPI)
driven by downscaled reanalysis data. The simulations were evaluated and interpreted …