Articles | Volume 11, issue 10
https://doi.org/10.5194/cp-11-1467-2015
© Author(s) 2015. 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-11-1467-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
How might the North American ice sheet influence the northwestern Eurasian climate?
P. Beghin
Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, UMR 8212, Gif-sur-Yvette, France
Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, UMR 8212, Gif-sur-Yvette, France
C. Dumas
Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, UMR 8212, Gif-sur-Yvette, France
M. Kageyama
Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, UMR 8212, Gif-sur-Yvette, France
Laboratoire de Glaciologie et de Géophysique de l'Environnement, CNRS-UJF, UMR 5183, Saint Martin d'Hères, France
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20 citations as recorded by crossref.
- The Alpine LGM in the boreal ice-sheets game G. Monegato et al. 10.1038/s41598-017-02148-7
- Holocene lowering of the Laurentide ice sheet affects North Atlantic gyre circulation and climate L. Gregoire et al. 10.1007/s00382-018-4111-9
- 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
- Linking Danube River activity to Alpine Ice-Sheet fluctuations during the last glacial (ca. 33–17 ka BP): Insights into the continental signature of Heinrich Stadials R. Martinez-Lamas et al. 10.1016/j.quascirev.2019.106136
- Numerical reconstructions of the penultimate glacial maximum Northern Hemisphere ice sheets: sensitivity to climate forcing and model parameters C. WEKERLE et al. 10.1017/jog.2016.45
- Timing and flow pattern of the Orta Glacier (European Alps) during the Last Glacial Maximum J. Braakhekke et al. 10.1111/bor.12427
- Climatic conditions between 19 and 12 ka in the eastern Pyrenees, and wider implications for atmospheric circulation patterns in Europe T. Reixach et al. 10.1016/j.quascirev.2021.106923
- Late Pleistocene glacial terminations accelerated by proglacial lakes M. Scherrenberg et al. 10.5194/cp-20-1761-2024
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- Holocene temperature variation recorded by branched glycerol dialkyl glycerol tetraethers in a loess-paleosol sequence from the north-eastern Tibetan Plateau T. Wang et al. 10.1007/s11707-023-1094-6
- Last Glacial loess in Europe: luminescence database and chronology of deposition M. Bosq et al. 10.5194/essd-15-4689-2023
- General Holocene warming trend in arid Central Asia indicated by soil isoprenoid tetraethers Y. Duan et al. 10.1016/j.gloplacha.2022.103879
- Millennial‐Scale Climate Oscillations Triggered by Deglacial Meltwater Discharge in Last Glacial Maximum Simulations Y. Romé et al. 10.1029/2022PA004451
- Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years S. Affolter et al. 10.1126/sciadv.aav3809
- The Ticino-Toce glacier system (Swiss-Italian Alps) in the framework of the Alpine Last Glacial Maximum S. Kamleitner et al. 10.1016/j.quascirev.2022.107400
- Dynamics and sources of last glacial aeolian deposition in southwest France derived from dune patterns, grain-size gradients and geochemistry, and reconstruction of efficient wind directions L. Sitzia et al. 10.1016/j.quascirev.2017.06.029
- Climate and ice sheet dynamics in Patagonia throughout marine isotope stages 2 and 3 A. Castillo-Llarena et al. 10.5194/cp-20-1559-2024
- Numerical reconstructions of the flow and basal conditions of the Rhine glacier, European Central Alps, at the Last Glacial Maximum D. Cohen et al. 10.5194/tc-12-2515-2018
- 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
2 citations as recorded by crossref.
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Short summary
The present study investigates the potential impact of the North American ice sheet on the surface mass balance of the Eurasian ice sheet through changes in the past glacial atmospheric circulation. Using an atmospheric circulation model and an ice-sheet model, we show that the albedo of the American ice sheet favors the growth of the Eurasian ice sheet, whereas the topography of the American ice sheet leads to more ablation over North Eurasia, and therefore to a smaller Eurasian ice sheet.
The present study investigates the potential impact of the North American ice sheet on the...