A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment
We present a new reconstruction of the Antarctic Ice Sheets between 20 ka BP and the
present day. Our reconstruction is derived using a numerical model to generate a physically …
present day. Our reconstruction is derived using a numerical model to generate a physically …
[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 …
Dynamics of the last glacial maximum Antarctic ice-sheet and its response to ocean forcing
NR Golledge, CJ Fogwill… - Proceedings of the …, 2012 - National Acad Sciences
Retreat of the Last Glacial Maximum (LGM) Antarctic ice sheet is thought to have been
initiated by changes in ocean heat and eustatic sea level propagated from the Northern …
initiated by changes in ocean heat and eustatic sea level propagated from the Northern …
Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet
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 …
current rates of mass loss, but assessing whether or not these processes are a natural part …
Hypolithic communities shape soils and organic matter reservoirs in the ice-free landscapes of East Antarctica
Abstract The soils of East Antarctica have no rhizosphere with the bulk of organo-mineral
interactions confined to the thin microbial and cryptogamic crusts that occur in open or …
interactions confined to the thin microbial and cryptogamic crusts that occur in open or …
Formation of subaerial taliks in Larsemann hills, princess Elizabeth land, East Antarctica
SV Popov, AS Boronina, AV Nemchinova… - Polar Science, 2024 - Elsevier
This study presents a mathematical model of heat and mass transfer for modelling the
formation and evolution of taliks in the upper subsurface of the Larsemann Hills in East …
formation and evolution of taliks in the upper subsurface of the Larsemann Hills in East …
Post-glacial regional climate variability along the East Antarctic coastal margin—evidence from shallow marine and coastal terrestrial records
We review the post-glacial climate variability along the East Antarctic coastline using
terrestrial and shallow marine geological records and compare these reconstructions with …
terrestrial and shallow marine geological records and compare these reconstructions with …
[HTML][HTML] Controls on subaerial erosion rates in Antarctica
Erosion rates offer insight on landscape development and the relative importance of
chemical and physical processes of weathering. Minimal chemical weathering makes …
chemical and physical processes of weathering. Minimal chemical weathering makes …
Soils of wet valleys in the larsemann hills and vestfold hills oases (Princess Elizabeth land, east Antarctica)
NS Mergelov - Eurasian soil science, 2014 - Springer
The properties and spatial distribution of soils and soil-like bodies in valleys of the coastal
Larsemann Hills and Vestfold Hills oases—poorly investigated in terms of the soil areas of …
Larsemann Hills and Vestfold Hills oases—poorly investigated in terms of the soil areas of …
High-resolution insights of physical properties of water columns of lakes at the Larsemann Hills, East Antarctica
During the Austral summer of 2022, a study was conducted to investigate the physical
properties of six lakes in the Larsemann Hills, East Antarctica. The lake water column's key …
properties of six lakes in the Larsemann Hills, East Antarctica. The lake water column's key …