Antarctic Peninsula Ice Sheet
Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves
... the sheet-shelf models may be attributed to a combination of differences in initialisation, inferred basal traction fields, and PSU3D not being as close to steady state as BISICLES following initialisation and ...
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Configuration of the Northern Antarctic Peninsula Ice Sheet at LGM based on a new synthesis of seabed imagery
... of ice domes, ice divides, and diverg- ing/converging flows help us to understand ice-sheet evolu- tion and ...of ice cores and marine drilling ...future ice- sheet ...
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Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
... the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum (LGM) through deglaciation to the present ...arctic Peninsula (AP) shelf indicate that the APIS was grounded to ...
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Glacier dynamics, ice mass unloading and bedrock response in the southern Antarctic Peninsula
... the Antarctic Peninsula (AP) have experienced rapid regional atmospheric and oceanic warming, leading to significant retreat and disintegration of ice shelves and rapid acceleration of mass discharge ...
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Detailed ice loss pattern in the northern Antarctic Peninsula: widespread decline driven by ice front retreats
... northern Antarctic Peninsula (nAP, < 66 ◦ S) is one of the most rapidly changing glaciated regions on earth, yet the spatial patterns of its ice mass loss at the glacier basin scale have to date ...
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Modelling the Antarctic Ice Sheet across the mid-Pleistocene transition – implications for Oldest Ice
... marine-based ice has a more slippery base as compared to ice above sea level, al- lowing for faster flowing marine outlet ...the ice–bedrock interface). The grid resolution resolves the major ...
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Glacial geomorphology of Marguerite Bay Palaeo-Ice stream, western Antarctic Peninsula
... marine ice-stream signatures available for scrutiny, and these data hold much potential for reconstructing former ice sheet dynamics, testing numerical ice sheet models, and ...
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Simultaneous solution for mass trends on the West Antarctic Ice Sheet
... The Antarctic Ice Sheet is the largest potential source of future sea-level ...West Antarctic Ice Sheet (WAIS) but with significant discrepancies between estimates, especially ...
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Future Antarctic bed topography and its implications for ice sheet dynamics
... the ice loading history and its short-term (centennial timescale) vis- coelastic response to the future ice load ...future ice load- ing to the evolution of future bed ...of ice thick- ness ...
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Modelling the evolution of the Antarctic ice sheet since the last interglacial
... the Antarctic Peninsula has not re- treated far enough, which is probably also due to the low res- olution of the ...Ross Ice Shelf is well modelled in ...Filchner–Ronne Ice Shelf has ...
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Mass balance of the Antarctic Ice Sheet from 1992 to 2017
... of ice sheet mass ...East Antarctic (EAIS), West Antarctic (WAIS), Antarctic Peninsula (APIS) and Antarctic (AIS) ice ...
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A 21 000-year record of fluorescent organic matter markers in the WAIS Divide ice core
... WD ice core fluorescent OM markers identified components used to better understand ecological influences in a changing climate, providing more information on the types of C produced than is currently reported in ...
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The Potsdam Parallel Ice Sheet Model (PISM-PIK) – Part 2: Dynamic equilibrium simulation of the Antarctic ice sheet
... of ice thickness to ...in ice thickness of not more than a couple of hundred meters (positive or neg- ative, ...Ross Ice Shelf, the Pine Island Glacier and the Filchner Ice Shelf, and the ...
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Dynamic Antarctic ice sheet during the early to mid-Miocene.
... the ice cliff height reaches 100 m, in water depths of 800 m [ ...that ice cliffs can reach before failing structurally [ ...total ice volume change between the cold and warmer climate simulations is ...
7
The Antarctic Ice Sheet response to glacial millennial-scale variability
... events. Ice-core records from the Greenland Ice Sheet (GrIS) dur- ing the LGP show the characteristic signal of DO events: a rapid warming of more than 10 K on decadal timescales fol- lowed by a slow ...
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The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
... as these glaciers were still connected with Evans Glacier in 2007. With an ice thickness of 268 m the main parts of the frontal glacier areas are floating. This agrees with the obser- vation of major frontal ...
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Antarctic ice sheet thickness estimation using the horizontal-to-vertical spectral ratio method with single-station seismic ambient noise
... the Antarctic ice sheet ...the ice sheet ...the ice thickness but, should be used with care since the shear-wave velocity varies at dif- ferent ...reliable ice thickness ...
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Seafloor geomorphology of western Antarctic Peninsula bays: a signature of ice flow behaviour
... Models showing geomorphic features have been pre- sented largely for the continental shelf in Antarctica (Well- ner et al., 2001; Canals et al., 2002; Evans et al., 2004; Dowdeswell et al., 2008; Graham et al., 2009), ...
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A comparison of modelled ice thickness and volume across the entire Antarctic Peninsula region
... Trinity Peninsula west of main divide TP-East Trinity Peninsula east of main divide GL-West Graham Land west of main divide GL-East Graham Land east of main divide PL-west Palmer Land west of main divide ...
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A comparison of modelled ice thickness and volume across the entire Antarctic Peninsula region
... Trinity Peninsula west of main divide TP-East Trinity Peninsula east of main divide GL-West Graham Land west of main divide GL-East Graham Land east of main divide PL-west Palmer Land west of main divide ...
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