Articles | Volume 12, issue 5
https://doi.org/10.5194/cp-12-1225-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1225-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
25 May 2016
Research article |
| 25 May 2016
The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle
Johan Liakka
CORRESPONDING AUTHOR
Biodiversity and Climate Research Centre, Senckenberg Gesellschaft für Naturforschung,
Senckenberganlage 25, 60325 Frankfurt am Main, Germany
Marcus Löfverström
National Center for Atmospheric Research, 1850 Table Mesa Drive, Boulder, Colorado, CO 80305, USA
Florence Colleoni
Centro Euro-Mediterraneo sui Cambiamenti Climatici, Via Franceschini 31, 40128 Bologna, Italy
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32 citations as recorded by crossref.
- Arctic warming induced by the Laurentide Ice Sheet topography J. Liakka & M. Lofverstrom 10.5194/cp-14-887-2018
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- Abrupt regime shifts in the North Atlantic atmospheric circulation over the last deglaciation M. Löfverström & J. Lora 10.1002/2017GL074274
- The rapid deglaciation of the Skagafjörður fjord, northern Iceland N. Andrés et al. 10.1111/bor.12341
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- Differences between the last two glacial maxima and implications for ice-sheet, δ18O, and sea-level reconstructions E. Rohling et al. 10.1016/j.quascirev.2017.09.009
- Penultimate Glacial Cycle glacier extent in the Iberian Peninsula: New evidence from the Serra da Estrela (Central System, Portugal) G. Vieira et al. 10.1016/j.geomorph.2021.107781
- Western Siberia experienced rapid shifts in moisture source and summer water balance during the last deglaciation and early Holocene O. Cowling et al. 10.1002/jqs.3386
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- The deglaciation of the Americas during the Last Glacial Termination D. Palacios et al. 10.1016/j.earscirev.2020.103113
- Last glacial inception trajectories for the Northern Hemisphere from coupled ice and climate modelling T. Bahadory et al. 10.5194/cp-17-397-2021
- On the limited ice intrusion in Alaska at the LGM M. Löfverström & J. Liakka 10.1002/2016GL071012
- Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach E. Bauer & A. Ganopolski 10.5194/cp-13-819-2017
- The importance of snow albedo for ice sheet evolution over the last glacial cycle M. Willeit & A. Ganopolski 10.5194/cp-14-697-2018
- Early Holocene Laurentide Ice Sheet Retreat Influenced Summer Atmospheric Circulation in Baffin Bay E. Thomas et al. 10.1029/2023GL103428
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- Investigating similarities and differences of the penultimate and last glacial terminations with a coupled ice sheet–climate model A. Quiquet & D. Roche 10.5194/cp-20-1365-2024
- Hypersensitivity of glacial summer temperatures in Siberia P. Bakker et al. 10.5194/cp-16-371-2020
- Late Pleistocene glacial terminations accelerated by proglacial lakes M. Scherrenberg et al. 10.5194/cp-20-1761-2024
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- Glacial erosion and Quaternary landscape development of the Eurasian Arctic H. Patton et al. 10.1016/j.earscirev.2024.104936
- Contrasting the Penultimate Glacial Maximum and the Last Glacial Maximum (140 and 21 ka) using coupled climate–ice sheet modelling V. Patterson et al. 10.5194/cp-20-2191-2024
- A sedimentary record from the Makarov Basin, Arctic Ocean, reveals changing middle to Late Pleistocene glaciation patterns W. Xiao et al. 10.1016/j.quascirev.2021.107176
- Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. 10.1029/2021GL096767
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- Isotopic Fingerprints of Ice‐Rafted Debris Offer New Constraints on Middle to Late Quaternary Arctic Circulation and Glacial History L. Dong et al. 10.1029/2020GC009019
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3 citations as recorded by crossref.
- Constraint on the penultimate glacial maximum Northern Hemisphere ice topography (≈140 kyrs BP) F. Colleoni et al. 10.1016/j.quascirev.2016.01.024
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Saved (preprint)
Latest update: 23 Nov 2024
Short summary
The present study explains why Scandinavia was ice-covered 20 000 years ago, while Siberia was mostly ice free. The authors show that the ice-sheet extent in Eurasia was to a large extent controlled by atmospheric circulation changes due to the ice sheet in North America. As the North American ice sheet becomes larger, it induces a cooling in Europe and a warming in Siberia: this climatic pattern forces the Eurasian ice sheet to migrate westward until it is centered over Scandinavia.
The present study explains why Scandinavia was ice-covered 20 000 years ago, while Siberia was...
