Holocene reconfiguration and readvance of the East Antarctic Ice Sheet. [PDF]
Greenwood SL +4 more
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High climate model dependency of Pliocene Antarctic ice-sheet predictions. [PDF]
Dolan AM +4 more
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Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions. [PDF]
Colleoni F +10 more
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Probabilistic inversion of expert assessments to inform projections about Antarctic ice sheet responses. [PDF]
Fuller RW, Wong TE, Keller K.
europepmc +1 more source
Rate-induced tipping in marine-based regions of the Antarctic ice sheet
Swierczek-Jereczek J +4 more
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Mass balance of the Greenland and Antarctic ice sheets from the 1970s to 2023. [PDF]
Otosaka IN +57 more
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Three-dimensional reconstruction of glacier-derived freshwater in East Antarctica using an end-member-independent hydrographic parameterization. [PDF]
Watanabe YW +6 more
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Related searches:
Changes in the West Antarctic Ice Sheet
Science, 1991The portion of the West Antarctic ice sheet that flows into the Ross Sea is thinning in some places and thickening in others. These changes are not caused by any current climatic change, but by the combination of a delayed response to the end of the last global glacial cycle and an internal instability. The near-future impact of the ice sheet on global
R B, Alley, I M, Whillans
openaire +2 more sources
Mass balance of the Antarctic ice sheet
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 2006The Antarctic contribution to sea-level rise has long been uncertain. While regional variability in ice dynamics has been revealed, a picture of mass changes throughout the continental ice sheet is lacking. Here, we use satellite radar altimetry to measure the elevation change of 72% of the grounded ice sheet during the period 1992–2003 ...
Wingham, D.J. +3 more
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Antarctica is the fifth largest continent on the Earth with an area of 14,200,000 km2. About 98% of the surface of Antarctica is covered by an ice sheet that is 2,000 m thick on average. The volume of the ice sheet has changed in the course of time and reached a maximum during the late Wisconsin (Weichselian) ice age about 20,000 years ago.
Gunter Faure, Teresa M. Mensing
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