Articles | Volume 15, issue 10
https://doi.org/10.5194/tc-15-4703-2021
© Author(s) 2021. 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-15-4703-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Oct 2021
Research article |
| 07 Oct 2021
| 07 Oct 2021
Lasting impact of winds on Arctic sea ice through the ocean's memory
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Bremerhaven, Germany
Laboratory for Regional Oceanography and Numerical Modeling,
Pilot National Laboratory for Marine Science and Technology, Qingdao, China
Sergey Danilov
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Bremerhaven, Germany
Department of Mathematics and Logistics, Jacobs University, Bremen, Germany
A. M. Obukhov Institute of Atmospheric Physics Russian Academy of Science, Moscow, Russia
Longjiang Mu
Laboratory for Ocean and Climate Dynamics, Pilot National Laboratory for Marine Science and Technology, Qingdao, China
Dmitry Sidorenko
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Bremerhaven, Germany
Claudia Wekerle
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Bremerhaven, Germany
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- Sea ice decline in the Eastern Arctic results in expansion of the freshened surface layer V. Rogozhin et al. 10.3389/fmars.2025.1558240
- The connection between sea ice dynamics enhancement and atmospheric circulation in the East Siberian Sea during spring D. Zhang et al. 10.1088/2515-7620/ad78bd
- Surface and Interior Dynamics of Arctic Seas Using Surface Quasi-Geostrophic Approach M. Umbert et al. 10.3390/rs15071722
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Latest update: 10 Jul 2025
Short summary
Using simulations, we found that changes in ocean freshwater content induced by wind perturbations can significantly affect the Arctic sea ice drift, thickness, concentration and deformation rates years after the wind perturbations. The impact is through changes in sea surface height and surface geostrophic currents and the most pronounced in warm seasons. Such a lasting impact might become stronger in a warming climate and implies the importance of ocean initialization in sea ice prediction.
Using simulations, we found that changes in ocean freshwater content induced by wind...
