Ice flow dynamics of the northwestern Laurentide Ice Sheet during the last deglaciation [PDF]
Reconstructions of palaeo-ice-stream activity provide insight into the processes governing ice stream evolution over millennial timescales. The northwestern sector of the Laurentide Ice Sheet experienced a period of rapid retreat driven by warming during
B. J. Stoker +11 more
doaj +1 more source
Atmospheric River Contributions to Ice Sheet Hydroclimate at the Last Glacial Maximum
Atmospheric rivers (ARs) are an important driver of surface mass balance over today's Greenland and Antarctic ice sheets. Using paleoclimate simulations with the Community Earth System Model, we find ARs also had a key influence on the extensive ice ...
Christopher B. Skinner +3 more
doaj +1 more source
Cosmogenic ages indicate no MIS 2 refugia in the Alexander Archipelago, Alaska [PDF]
The late-Pleistocene history of the coastal Cordilleran Ice Sheet remains relatively unstudied compared to chronologies of the Laurentide Ice Sheet. Yet accurate reconstructions of Cordilleran Ice Sheet extent and the timing of ice retreat along the ...
C. K. Walcott +4 more
doaj +1 more source
Eastern Beringia and beyond: Late Wisconsinan and Holocene landscape dynamics along the Yukon Coastal Plain, Canada [PDF]
Terrestrial permafrost archives along the Yukon Coastal Plain (northwest Canada) have recorded landscape development and environmental change since the Late Wisconsinan at the interface of unglaciated Beringia (i.e.
Fritz, Michael +6 more
core +1 more source
Ice streams in the Laurentide Ice Sheet: a new mapping inventory [PDF]
Rapidly flowing ice streams dominate the drainage of continental ice sheets and are a key component of their mass balance. Due to their potential impact on sea level, their activity in the Antarctic and Greenland Ice Sheets has undergone detailed scrutiny in recent decades.
Margold, M. +3 more
openaire +3 more sources
Arctic ice export events and their potential impact on global climate during the late Pleistocene [PDF]
Ice sheets in the North American Arctic and, to a lesser extent, those in northern Eurasia calved large quantities of icebergs that drifted through Fram Strait into the Greenland Sea several times during the late Pleistocene.
Bischof, J. F. +4 more
core +3 more sources
Fossil Java Sea corals record Laurentide ice sheet disappearance [PDF]
Abstract The Laurentide ice sheet was the largest late Pleistocene ice mass and the largest contributor to Holocene pre-industrial sea-level rise. While glaciological dates suggest final ice sheet melting between 8 and 6 ka, inversion of sea-level data indicates deglaciation at ca. 7 ka.
Mann, Thomas +10 more
openaire +2 more sources
Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle [PDF]
We present modelling results of the atmospheric circulation at the cold periods of marine isotope stage 5b (MIS 5b), MIS 4 and the Last Glacial Maximum (LGM), as well as the interglacial.
M. Löfverström +3 more
doaj +1 more source
Northern Hemisphere ice sheet and ocean interactions during the last glacial period in a coupled ice sheet–climate model [PDF]
This study examines the interactions between the Northern Hemisphere ice sheets and the ocean during the last glacial period. Using the iLOVECLIM climate model of intermediate complexity and the GRISLI ice sheet model, we explore the consequences of an ...
L. Abot, A. Quiquet, C. Waelbroeck
doaj +1 more source
Climatic warming following the Last Glacial Maximum caused the southern Laurentide Ice Sheet (LIS) to begin ∼2,000‐year cycles of retreat and readvance whose cause remains ambiguous.
Andrew D. Wickert +7 more
doaj +1 more source

