[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
[HTML][HTML] Glacial erosion and Quaternary landscape development of the Eurasian Arctic
Multiple ice age cycles spanning the last three million years have fundamentally transformed
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …
[HTML][HTML] Modelling last glacial cycle ice dynamics in the Alps
The European Alps, the cradle of pioneering glacial studies, are one of the regions where
geological markers of past glaciations are most abundant and well-studied. Such conditions …
geological markers of past glaciations are most abundant and well-studied. Such conditions …
Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion
Climate variations cause ice sheets to retreat and advance, raising or lowering sea level by
metres to decametres. The basic relationship is unambiguous, but the timing, magnitude and …
metres to decametres. The basic relationship is unambiguous, but the timing, magnitude and …
East Antarctic ice sheet most vulnerable to Weddell Sea warming
Abstract Models predict considerable spatial variability in the magnitude of future climate
change around Antarctica, suggesting that some sectors of the continent may be more …
change around Antarctica, suggesting that some sectors of the continent may be more …
Numerical simulations of the Cordilleran ice sheet through the last glacial cycle
After more than a century of geological research, the Cordilleran ice sheet of North America
remains among the least understood in terms of its former extent, volume, and dynamics …
remains among the least understood in terms of its former extent, volume, and dynamics …
Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma
The geometry of Antarctic ice sheets during warm periods of the geological past is difficult to
determine from geological evidence, but is important to know because such reconstructions …
determine from geological evidence, but is important to know because such reconstructions …
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling
During the Last Glacial Maximum (LGM), glaciers in the Alps reached a maximum extent,
and broad sections of the foreland were covered by ice. In this study, we simulated the …
and broad sections of the foreland were covered by ice. In this study, we simulated the …
Positive degree-day sums in the Alps: a direct link between glacier melt and international climate policy
Annual balances of eight alpine glaciers were slightly negative for 1961–90 and highly
negative for 1991–2018. We explain this by changes in positive degree-day sums and …
negative for 1991–2018. We explain this by changes in positive degree-day sums and …
Collapse of the last Eurasian Ice Sheet in the North Sea modulated by combined processes of ice flow, surface melt, and marine ice sheet instabilities
The record of the confluence and collapse of the British‐Irish Ice Sheet and the
Fennoscandian Ice Sheet is obscured by the North Sea, hindering reconstructions of the …
Fennoscandian Ice Sheet is obscured by the North Sea, hindering reconstructions of the …