Proxy records from across the Southern Hemisphere show significant local to regional scale
variability in climatic and environmental conditions during late Marine Isotope Stage 3 and …

Abstract In southern South America, well-dated glacial geomorphological records constrain
the last glacial cycle across much of the former Patagonian Ice Sheet, but its northeastern …

Numerical glacier models applied to moraine chronologies provide an opportunity to
quantify past climate change. Here we apply a two-dimensional coupled mass balance–ice …

Determining how and why eruptive outputs are modulated by the loading and unloading of
ice is key to understanding whether ongoing and accelerating deglaciation across mid-to …

Robust geomorphological interpretations of ice-marginal glacial, meltwater and palaeolake
landforms are needed to constrain models of landform evolution that can be used to …

Studying the retreat of the Patagonian Ice Sheet (PIS) during the last deglaciation represents
an important opportunity to understand how ice sheets outside the polar regions have …

Climatic variability across a large fraction of the Southern Hemisphere is controlled by the
Southern Annular Mode and associated latitudinal shifts in the Southern Westerly Wind belt …

The cold climate events of the Upper Cenozoic greatly modified the landscape of Patagonia,
where a large number of relicts and active landforms of glacial, periglacial and paraglacial …

The effect of post-depositional processing on the preservation of snow nitrate isotopes at
Summit, Greenland, remains a subject of debate and is relevant to the quantitative …

The precise environmental mechanisms controlling Quaternary glacial cycles remain
ambiguous. To address this problem, it is critical to better comprehend the drivers of spatio …