Response of the East Antarctic Ice Sheet to past and future climate change
Abstract The East Antarctic Ice Sheet contains the vast majority of Earth's glacier ice (about
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …
52 metres sea-level equivalent), but is often viewed as less vulnerable to global warming …
[HTML][HTML] The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE)
We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
The Weddell Gyre, Southern Ocean: present knowledge and future challenges
Abstract The Weddell Gyre (WG) is one of the main oceanographic features of the Southern
Ocean south of the Antarctic Circumpolar Current which plays an influential role in global …
Ocean south of the Antarctic Circumpolar Current which plays an influential role in global …
The sensitivity of the Antarctic ice sheet to a changing climate: Past, present, and future
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 …
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
[HTML][HTML] Antarctic ice rises and rumples: Their properties and significance for ice-sheet dynamics and evolution
Locally grounded features in ice shelves, called ice rises and rumples, play a key role
buttressing discharge from the Antarctic Ice Sheet and regulating its contribution to sea level …
buttressing discharge from the Antarctic Ice Sheet and regulating its contribution to sea level …
[HTML][HTML] A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum
A robust understanding of Antarctic Ice Sheet deglacial history since the Last Glacial
Maximum is important in order to constrain ice sheet and glacial-isostatic adjustment …
Maximum is important in order to constrain ice sheet and glacial-isostatic adjustment …
Stability of the Antarctic Ice Sheet during the pre-industrial Holocene
The rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …
[HTML][HTML] Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
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 …
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …
Antarctic sedimentary basins and their influence on ice‐sheet dynamics
Abstract Knowledge of Antarctica's sedimentary basins builds our understanding of the
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …
[HTML][HTML] Reconstruction of changes in the Amundsen Sea and Bellingshausen sea sector of the West Antarctic ice sheet since 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) …
since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) …