The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new map** inventory that includes previously hypothesised ice …

We measure the grounding line retreat of glaciers draining the Amundsen Sea sector of
West Antarctica using Earth Remote Sensing (ERS‐1/2) satellite radar interferometry from …

Resting atop a deep marine basin, the West Antarctic Ice Sheet has long been considered
prone to instability. Using a numerical model, we investigated the sensitivity of Thwaites …

Pine Island Glacier has thinned and accelerated over recent decades, significantly
contributing to global sea-level rise. Increased oceanic melting of its ice shelf is thought to …

Over the past decade, ice loss from the Greenland Ice Sheet increased as a result of both
increased surface melting and ice discharge to the ocean,. The latter is controlled by the …

The stability of marine ice sheets grounded on beds that slope upwards in the overall
direction of flow is investigated numerically in two horizontal dimensions. We give examples …

This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Glacier terminus changes are one of the hallmarks of worldwide glacier change, and thus,
there is significant focus on the controls and limits to retreat in the literature. Here we use the …