Articles | Volume 17, issue 1
Research article
12 Jan 2021
Research article |  | 12 Jan 2021

Can we reconstruct the formation of large open-ocean polynyas in the Southern Ocean using ice core records?

Hugues Goosse, Quentin Dalaiden, Marie G. P. Cavitte, and Liping Zhang

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Earth Syst. Sci. Data Discuss.,,, 2022
Revised manuscript under review for ESSD
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Internal climate variability and spatial temperature correlations during the past 2000 years
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Clim. Past, 18, 2523–2544,,, 2022
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Influence of fast ice on future ice shelf melting in the Totten Glacier area, East Antarctica
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Cited articles

Abram, N. J., Wolff, E. W., and Curran, M. A. J.: A review of sea ice proxy information from polar ice cores, Quaternary Sci. Rev., 79, 168–183,, 2013. 
Abram, N. J., Mulvaney, R., Vimeux, F., Phipps, S. J., Turner, J., and England, M. H.: Evolution of the Southern Annular Mode during the past millennium, Nat. Clim. Change, 4, 564–569,, 2014. 
Badgeley, J. A., Steig, E. J., Hakim, G. J., and Fudge, T. J.: Greenland temperature and precipitation over the last 20 000 years using data assimilation, Clim. Past, 16, 1325–1346,, 2020. 
Short summary
Polynyas are ice-free oceanic areas within the sea ice pack. Small polynyas are regularly observed in the Southern Ocean, but large open-ocean polynyas have been rare over the past decades. Using records from available ice cores in Antarctica, we reconstruct past polynya activity and confirm that those events have also been rare over the past centuries, but the information provided by existing data is not sufficient to precisely characterize the timing of past polynya opening.