Articles | Volume 15, issue 3
https://doi.org/10.5194/cp-15-957-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-15-957-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Jun 2019
Research article |
| 04 Jun 2019
| 04 Jun 2019
Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model
Jorge Alvarez-Solas
CORRESPONDING AUTHOR
Departamento de Física de la Tierra y Astrofísica, Facultad de Ciencias Físicas, Universidad Complutense de Madrid (UCM), Madrid, Spain
Instituto de Geociencias (UCM-CSIC), Madrid, Spain
Rubén Banderas
Departamento de Física de la Tierra y Astrofísica, Facultad de Ciencias Físicas, Universidad Complutense de Madrid (UCM), Madrid, Spain
Instituto de Geociencias (UCM-CSIC), Madrid, Spain
Alexander Robinson
Departamento de Física de la Tierra y Astrofísica, Facultad de Ciencias Físicas, Universidad Complutense de Madrid (UCM), Madrid, Spain
Instituto de Geociencias (UCM-CSIC), Madrid, Spain
Marisa Montoya
Departamento de Física de la Tierra y Astrofísica, Facultad de Ciencias Físicas, Universidad Complutense de Madrid (UCM), Madrid, Spain
Instituto de Geociencias (UCM-CSIC), Madrid, Spain
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Cited
14 citations as recorded by crossref.
- Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea N. El bani Altuna et al. 10.1038/s43247-021-00264-x
- Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day C. Batchelor et al. 10.1038/s41586-023-05876-1
- Genetic and demographic signatures accompanying the evolution of the selfing syndrome inDaphne kiusiana, an evergreen shrub E. Han et al. 10.1093/aob/mcac142
- Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions J. Blasco et al. 10.5194/tc-15-215-2021
- Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3 I. Tabone et al. 10.5194/tc-13-1911-2019
- The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
- Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al. 10.1016/j.quascirev.2020.106314
- Collapse of the Last Eurasian Ice Sheet in the North Sea Modulated by Combined Processes of Ice Flow, Surface Melt, and Marine Ice Sheet Instabilities N. Gandy et al. 10.1029/2020JF005755
- The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet H. Sejrup et al. 10.1038/s43247-022-00447-0
- Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. 10.5194/cp-20-187-2024
- Depositional architecture and aggradation rates of sand-rich, supercritical alluvial fans: Control by autogenic processes or high-frequency climatic oscillations? J. Winsemann et al. 10.1016/j.sedgeo.2022.106238
- An ice–climate oscillatory framework for Dansgaard–Oeschger cycles L. Menviel et al. 10.1038/s43017-020-00106-y
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
- Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period I. Tabone et al. 10.5194/cp-15-593-2019
12 citations as recorded by crossref.
- Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea N. El bani Altuna et al. 10.1038/s43247-021-00264-x
- Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day C. Batchelor et al. 10.1038/s41586-023-05876-1
- Genetic and demographic signatures accompanying the evolution of the selfing syndrome inDaphne kiusiana, an evergreen shrub E. Han et al. 10.1093/aob/mcac142
- Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions J. Blasco et al. 10.5194/tc-15-215-2021
- Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3 I. Tabone et al. 10.5194/tc-13-1911-2019
- The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
- Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al. 10.1016/j.quascirev.2020.106314
- Collapse of the Last Eurasian Ice Sheet in the North Sea Modulated by Combined Processes of Ice Flow, Surface Melt, and Marine Ice Sheet Instabilities N. Gandy et al. 10.1029/2020JF005755
- The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet H. Sejrup et al. 10.1038/s43247-022-00447-0
- Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. 10.5194/cp-20-187-2024
- Depositional architecture and aggradation rates of sand-rich, supercritical alluvial fans: Control by autogenic processes or high-frequency climatic oscillations? J. Winsemann et al. 10.1016/j.sedgeo.2022.106238
- An ice–climate oscillatory framework for Dansgaard–Oeschger cycles L. Menviel et al. 10.1038/s43017-020-00106-y
2 citations as recorded by crossref.
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
- Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period I. Tabone et al. 10.5194/cp-15-593-2019
Latest update: 19 Nov 2024
Short summary
The last glacial period was marked by the existence of of abrupt climatic changes; it is generally accepted that the presence of ice sheets played an important role in their occurrence. While an important effort has been made to investigate the dynamics and evolution of the Laurentide ice sheet during this period, the Eurasian ice sheet (EIS) has not received much attention. Here we investigate the response of the EIS to millennial-scale climate variability using a hybrid 3-D ice-sheet model.
The last glacial period was marked by the existence of of abrupt climatic changes; it is...
