The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

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 …

Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …

The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Ice flow models used to project the mass balance of ice sheets in Greenland and Antarctica
usually rely on the Shallow Ice Approximation (SIA) and the Shallow‐Shelf Approximation …

The shallow shelf approximation, a balance of membrane stresses for ice flow, is an effective
“sliding law” for ice sheet modeling. Our use of it as a sliding law becomes a standard model …

Predictions of marine ice-sheet behaviour require models able to simulate grounding-line
migration. We present results of an intercomparison experiment for plan-view marine ice …

Predictions of marine ice-sheet behaviour require models that are able to robustly simulate
grounding line migration. We present results of an intercomparison exercise for marine ice …

Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …