It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …

We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …

Antarctic volume changes during the past 21 thousand years are smaller than previously
thought, and here we construct an ice sheet history that drives a forward model prediction of …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

Marine and terrestrial geological and marine geophysical data that constrain deglaciation
since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) …

Dynamical changes in contemporary ice sheets account for significant proportions of their
current rates of mass loss, but assessing whether or not these processes are a natural part …

The Antarctic Peninsula region is currently undergoing rapid environmental change,
resulting in the thinning, acceleration and recession of glaciers and the sequential collapse …

Abstract The Weddell Sea sector is one of the main formation sites for Antarctic Bottom
Water and an outlet for about one fifth of Antarctica's continental ice volume. Over the last …

The Amundsen Sea Embayment (ASE) drains approximately 35% of the West Antarctic Ice
Sheet (WAIS) and is one of the most rapidly changing parts of the cryosphere. In order to …

The Antarctic Circumpolar Current is one of the key components of ocean circulation, and a
knowledge of its isotopic composition is essential to the use of neodymium (Nd) isotopes to …