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 …
The early Holocene sea level rise
The causes, anatomy and consequences of the early Holocene sea level rise (EHSLR) are
reviewed. The rise, of ca 60m, took place over most of the Earth as the volume of the oceans …
reviewed. The rise, of ca 60m, took place over most of the Earth as the volume of the oceans …
Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model
WR Peltier, DF Argus… - Journal of Geophysical …, 2015 - Wiley Online Library
A new model of the last deglaciation event of the Late Quaternary ice age is here described
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level …
DF Argus, WR Peltier, R Drummond… - Geophysical Journal …, 2014 - academic.oup.com
ABSTRACT A new model of the deglaciation history of Antarctica over the past 25 kyr has
been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its …
been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its …
Millennial-scale variability in Antarctic ice-sheet discharge during the last deglaciation
Our understanding of the deglacial evolution of the Antarctic Ice Sheet (AIS) following the
Last Glacial Maximum (26,000–19,000 years ago) is based largely on a few well-dated but …
Last Glacial Maximum (26,000–19,000 years ago) is based largely on a few well-dated but …
Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation
AE Carlson, PU Clark - Reviews of Geophysics, 2012 - Wiley Online Library
We review and synthesize the geologic record that constrains the sources of sea level rise
and freshwater discharge to the global oceans associated with retreat of ice sheets during …
and freshwater discharge to the global oceans associated with retreat of ice sheets during …
Submarine glacial landforms and rates of ice-stream collapse
The rate of deglacial ice-sheet retreat across polar continental shelves, and possible ice-
stream collapse and sea-level rise, has been much debated. High-resolution imagery of …
stream collapse and sea-level rise, has been much debated. High-resolution imagery of …
[HTML][HTML] Retreat history of the East Antarctic Ice Sheet since the last glacial maximum
Abstract The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and
documenting its evolution since the Last Glacial Maximum (LGM) is important for …
documenting its evolution since the Last Glacial Maximum (LGM) is important for …
Retreat of the East Antarctic ice sheet during the last glacial termination
The retreat of the East Antarctic ice sheet at the end of the last glacial period has been
attributed to both sea-level rise and warming of the ocean at the margin of the ice sheet, but …
attributed to both sea-level rise and warming of the ocean at the margin of the ice sheet, but …
Antarctic palaeo-ice streams
We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …
ice streams on the continental shelf of Antarctica and use this information to investigate …