Articles | Volume 15, issue 3
https://doi.org/10.5194/cp-15-957-2019
https://doi.org/10.5194/cp-15-957-2019
Research article
 | 
04 Jun 2019
Research article |  | 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, Rubén Banderas, Alexander Robinson, and Marisa Montoya

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Cited articles

Åkesson, H., Morlighem, M., Nisancioglu, K. H., Svendsen, J. I., and Mangerud, J.: Atmosphere-driven ice sheet mass loss paced by topography: Insights from modelling the south-western Scandinavian Ice Sheet, Quaternary Sci. Rev., 195, 32–47, 2018. a
Alley, R. B., Clark, P. U., Huybrechts, P., and Joughin, I.: The deglaciation of the Northern Hemisphere: a global perspective, Annu. Rev. Earth Pl. Sc., 27, 149–182, https://doi.org/10.1146/annurev.earth.27.1.149, 1999. a
Alvarez-Solas, J.: Glacial Fennoscandian GRISLI-UCM simulations, https://doi.org/10.17605/OSF.IO/3KFUA, 2019. a
Alvarez-Solas, J., Charbit, S., Ritz, C., Paillard, D., Ramstein, G., and Dumas, C.: Links between ocean temperature and iceberg discharge during Heinrich events, Nat. Geosci., 3, 122–126, https://doi.org/10.1038/ngeo752, 2010. a
Alvarez-Solas, J., Charbit, S., Ramstein, G., Paillard, D., Dumas, C., Ritz, C., and Roche, D. M.: Millennial-scale oscillations in the Southern Ocean in response to atmospheric CO2 increase, Global Planet. Change, 76, 128–136, 2011a. a
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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.