Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model
WR Peltier, DF Argus… - Journal of Geophysical …, 2015 - Wiley Online Library
A new model of the last deglaciation event of the Late Quaternary ice age is here described
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
[HTML][HTML] Sea ice variability in the North Atlantic subpolar gyre throughout the last interglacial
Abstract The Last Interglacial period, Marine Isotope Stage 5e (MIS 5e∼ 116–128 ka), is
thought to have had a warmer, but less stable climate than the present interglacial. One key …
thought to have had a warmer, but less stable climate than the present interglacial. One key …
The demise of the Last Interglacial recorded in isotopically dated speleothems from the Alps
The transition from interglacial to glacial climate has attracted much attention in
paleoclimatic research, partly because orbital forcing dictates that such a return to a new ice …
paleoclimatic research, partly because orbital forcing dictates that such a return to a new ice …
The importance of Canadian Arctic Archipelago gateways for glacial expansion in Scandinavia
The last glacial cycle began around 116,000 years before present during a period with low
incoming solar radiation in Northern Hemisphere summer. Following the glacial inception in …
incoming solar radiation in Northern Hemisphere summer. Following the glacial inception in …
Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system
R Calov, A Ganopolski, M Claussen, V Petoukhov… - Climate Dynamics, 2005 - Springer
We study the mechanisms of glacial inception by using the Earth system model of
intermediate complexity, CLIMBER-2, which encompasses dynamic modules of the …
intermediate complexity, CLIMBER-2, which encompasses dynamic modules of the …
Orbital forcing of Arctic climate: mechanisms of climate response and implications for continental glaciation
CS Jackson, AJ Broccoli - Climate Dynamics, 2003 - Springer
Progress in understanding how terrestrial ice volume is linked to Earth's orbital configuration
has been impeded by the cost of simulating climate system processes relevant to glaciation …
has been impeded by the cost of simulating climate system processes relevant to glaciation …
Climate model tests of the anthropogenic influence on greenhouse-induced climate change: the role of early human agriculture, industrialization, and vegetation …
S Vavrus, WF Ruddiman, JE Kutzbach - Quaternary Science Reviews, 2008 - Elsevier
We test the early anthropogenic hypothesis that greenhouse-gas emissions produced by
early agricultural activities in recent millennia kept the climate warmer than its natural level …
early agricultural activities in recent millennia kept the climate warmer than its natural level …
[HTML][HTML] Progress in paleoclimate modeling
Progress in Paleoclimate Modeling in: Journal of Climate Volume 19 Issue 20 (2006) Jump
to Content Jump to Main Navigation Logo Logo Logo Logo Logo Logo JOURNALS Artificial …
to Content Jump to Main Navigation Logo Logo Logo Logo Logo Logo JOURNALS Artificial …
Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks
We present transient simulations of the last glacial inception using the Earth system model
CLIMBER-X with dynamic vegetation, interactive ice sheets, and visco-elastic solid Earth …
CLIMBER-X with dynamic vegetation, interactive ice sheets, and visco-elastic solid Earth …
Sensitivity of glacial inception to orbital and greenhouse gas climate forcing
G Vettoretti, WR Peltier - Quaternary Science Reviews, 2004 - Elsevier
Attempts to model climate system behaviour during the initiation of the last ice age provide a
further framework in which to test the quality of the global climate models (GCMs) that are …
further framework in which to test the quality of the global climate models (GCMs) that are …