Articles | Volume 17, issue 1
https://doi.org/10.5194/tc-17-407-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-17-407-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Jan 2023
Research article |
| 31 Jan 2023
| 31 Jan 2023
Modulation of the seasonal cycle of the Antarctic sea ice extent by sea ice processes and feedbacks with the ocean and the atmosphere
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Sofia Allende Contador
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Cecilia M. Bitz
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
Edward Blanchard-Wrigglesworth
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
Clare Eayrs
Korea Polar Research Institute, Incheon, South Korea
Thierry Fichefet
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Kenza Himmich
Laboratoire d'Océanographie et du Climat
(LOCEAN-IPSL), Sorbonne Université, CNRS, IRD, MNHN, Paris, France
Pierre-Vincent Huot
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
François Klein
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Sylvain Marchi
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
François Massonnet
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Bianca Mezzina
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Charles Pelletier
European Centre for Medium-Range Weather Forecasts, Bonn, Germany
Lettie Roach
NASA Goddard Institute for Space Studies, New York, NY, USA
Center for Climate Systems Research, Columbia University, New York, NY, USA
Martin Vancoppenolle
Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
Nicole P. M. van Lipzig
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
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Cited
5 citations as recorded by crossref.
- Signature of the stratosphere–troposphere coupling on recent record-breaking Antarctic sea-ice anomalies R. Cordero et al. 10.5194/tc-17-4995-2023
- Dynamic Thresholding Fully Automated sea ice extraction and classification methods based on multi-source remote-sensing data in the Yellow sea and Bohai sea regions J. Xu et al. 10.1016/j.asr.2024.05.073
- The sea ice component of GC5: coupling SI3 to HadGEM3 using conductive fluxes E. Blockley et al. 10.5194/gmd-17-6799-2024
- The role of atmospheric conditions in the Antarctic sea ice extent summer minima B. Mezzina et al. 10.5194/tc-18-3825-2024
- Impact of ocean vertical-mixing parameterization on Arctic sea ice and upper-ocean properties using the NEMO-SI3 model S. Allende et al. 10.5194/gmd-17-7445-2024
5 citations as recorded by crossref.
- Signature of the stratosphere–troposphere coupling on recent record-breaking Antarctic sea-ice anomalies R. Cordero et al. 10.5194/tc-17-4995-2023
- Dynamic Thresholding Fully Automated sea ice extraction and classification methods based on multi-source remote-sensing data in the Yellow sea and Bohai sea regions J. Xu et al. 10.1016/j.asr.2024.05.073
- The sea ice component of GC5: coupling SI3 to HadGEM3 using conductive fluxes E. Blockley et al. 10.5194/gmd-17-6799-2024
- The role of atmospheric conditions in the Antarctic sea ice extent summer minima B. Mezzina et al. 10.5194/tc-18-3825-2024
- Impact of ocean vertical-mixing parameterization on Arctic sea ice and upper-ocean properties using the NEMO-SI3 model S. Allende et al. 10.5194/gmd-17-7445-2024
Latest update: 23 Nov 2024
Short summary
Using idealized sensitivity experiments with a regional atmosphere–ocean–sea ice model, we show that sea ice advance is constrained by initial conditions in March and the retreat season is influenced by the magnitude of several physical processes, in particular by the ice–albedo feedback and ice transport. Atmospheric feedbacks amplify the response of the winter ice extent to perturbations, while some negative feedbacks related to heat conduction fluxes act on the ice volume.
Using idealized sensitivity experiments with a regional atmosphere–ocean–sea ice model, we show...
