A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent
An ice sheet model was constrained to reconstruct the evolution of the Greenland Ice Sheet
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …
History of the Greenland Ice Sheet: paleoclimatic insights
Paleoclimatic records show that the Greenland Ice Sheet consistently has lost mass in
response to warming, and grown in response to cooling. Such changes have occurred even …
response to warming, and grown in response to cooling. Such changes have occurred even …
[LIBRO][B] Reconstructing quaternary environments
This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …
and updated to provide a new account of the history and scale of environmental changes …
The Greenland Ice Sheet during the past 300,000 years: A review
The Greenland ice sheet's response to climate change is a major issue in the climate
debate. This report reviews existing evidence on how the ice sheet margins reacted to …
debate. This report reviews existing evidence on how the ice sheet margins reacted to …
A new Holocene relative sea level curve for the South Shetland Islands, Antarctica
Precise relative sea level (RSL) data are important for inferring regional ice sheet histories,
as well as hel** to validate numerical models of ice sheet evolution and glacial isostatic …
as well as hel** to validate numerical models of ice sheet evolution and glacial isostatic …
Using proglacial-threshold lakes to constrain fluctuations of the Jakobshavn Isbræ ice margin, western Greenland, during the Holocene
The future response of the Greenland Ice Sheet (GIS) and its potential contribution to sea
level rise are uncertain. Rapid changes of Greenland's outlet glaciers over the past decade …
level rise are uncertain. Rapid changes of Greenland's outlet glaciers over the past decade …
[HTML][HTML] Glacier response to the Little Ice Age during the Neoglacial cooling in Greenland
Abstract In the Northern Hemisphere, an insolation driven Early to Middle Holocene Thermal
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …
Isolation basins, sea-level changes and the Holocene history of the Greenland Ice Sheet
Isolation basins are natural topographic depressions that at various times in their history
may be connected to or isolated from the sea by changes in relative sea-level (RSL). They …
may be connected to or isolated from the sea by changes in relative sea-level (RSL). They …
The Greenland Ice Sheet during the last glacial cycle: Current ice loss and contribution to sea-level rise from a palaeoclimatic perspective
Abstract During the Last Interglacial (LIG) period, between 130 and 116 thousand years
before present (ka BP), the Greenland Ice Sheet (GrIS) was considerably reduced in size …
before present (ka BP), the Greenland Ice Sheet (GrIS) was considerably reduced in size …
Sedimentary coastal cliff erosion in Greenland
Climate change will increase the duration of annual sea‐ice‐free periods and shift
precipitation patterns across the Arctic. Those factors are likely to increase erosion rates …
precipitation patterns across the Arctic. Those factors are likely to increase erosion rates …