Future Atlantification of the European Arctic limited under sustained global warming

Abstract Atlantification is an ongoing oceanic phenomenon characterised by the expansion of the typical Atlantic domain towards the Arctic, driving rapid oceanic and ecological changes in the European Arctic. Using reanalyses and a multi-model ensemble of unperturbed and transient preindustrial, his...

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Main Authors: Francesco De Rovere, Matteo Mastropierro, Johann H. Jungclaus, Myriam Khodri, Angelo Rubino, Davide Zanchettin
Format: Article
Language:English
Published: Nature Portfolio 2025-08-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-025-16161-8
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author Francesco De Rovere
Matteo Mastropierro
Johann H. Jungclaus
Myriam Khodri
Angelo Rubino
Davide Zanchettin
author_facet Francesco De Rovere
Matteo Mastropierro
Johann H. Jungclaus
Myriam Khodri
Angelo Rubino
Davide Zanchettin
author_sort Francesco De Rovere
collection DOAJ
description Abstract Atlantification is an ongoing oceanic phenomenon characterised by the expansion of the typical Atlantic domain towards the Arctic, driving rapid oceanic and ecological changes in the European Arctic. Using reanalyses and a multi-model ensemble of unperturbed and transient preindustrial, historical and future-scenario simulations, this study shows that modern Atlantification possibly initiated in the late nineteenth century, preceded by several “Arctification” episodes in the preindustrial millennium. In the historical period, Atlantification and pan-Arctic warming superposed constructively to drive upper-ocean warming and salinification in the Barents Sea. Modern Atlantification is projected to continue in the next few decades, fully revealing its exceptional character in the context of the past millennium. However, Atlantification halts during the second half of the twenty-first century, decoupling from pan-Arctic warming. The northward expansion of the Atlantic domain is hindered by the onset of a damping mechanism where the Atlantic-Arctic density gradient increases progressively, which sustains a countercurrent by baroclinic adjustment pushing the Arctic polar front southward. As the evolution of this density gradient is intertwined with the retreat of the sea-ice edge, a late-summer ice-free Barents Sea may mark the end of modern Atlantification.
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spelling doaj-art-6ed7bb6c38a54c0f9dc110559499c8df2025-08-24T11:21:30ZengNature PortfolioScientific Reports2045-23222025-08-0115111410.1038/s41598-025-16161-8Future Atlantification of the European Arctic limited under sustained global warmingFrancesco De Rovere0Matteo Mastropierro1Johann H. Jungclaus2Myriam Khodri3Angelo Rubino4Davide Zanchettin5Department of Environmental Sciences, Informatics and Statistics, Ca’ Foscari University of VeniceDepartment of Environmental Sciences, Informatics and Statistics, Ca’ Foscari University of VeniceMax-Planck-Institut für MeteorologieLOCEAN-IPSL, Sorbonne Université/CNRS/IRD/MNHNDepartment of Environmental Sciences, Informatics and Statistics, Ca’ Foscari University of VeniceDepartment of Environmental Sciences, Informatics and Statistics, Ca’ Foscari University of VeniceAbstract Atlantification is an ongoing oceanic phenomenon characterised by the expansion of the typical Atlantic domain towards the Arctic, driving rapid oceanic and ecological changes in the European Arctic. Using reanalyses and a multi-model ensemble of unperturbed and transient preindustrial, historical and future-scenario simulations, this study shows that modern Atlantification possibly initiated in the late nineteenth century, preceded by several “Arctification” episodes in the preindustrial millennium. In the historical period, Atlantification and pan-Arctic warming superposed constructively to drive upper-ocean warming and salinification in the Barents Sea. Modern Atlantification is projected to continue in the next few decades, fully revealing its exceptional character in the context of the past millennium. However, Atlantification halts during the second half of the twenty-first century, decoupling from pan-Arctic warming. The northward expansion of the Atlantic domain is hindered by the onset of a damping mechanism where the Atlantic-Arctic density gradient increases progressively, which sustains a countercurrent by baroclinic adjustment pushing the Arctic polar front southward. As the evolution of this density gradient is intertwined with the retreat of the sea-ice edge, a late-summer ice-free Barents Sea may mark the end of modern Atlantification.https://doi.org/10.1038/s41598-025-16161-8
spellingShingle Francesco De Rovere
Matteo Mastropierro
Johann H. Jungclaus
Myriam Khodri
Angelo Rubino
Davide Zanchettin
Future Atlantification of the European Arctic limited under sustained global warming
Scientific Reports
title Future Atlantification of the European Arctic limited under sustained global warming
title_full Future Atlantification of the European Arctic limited under sustained global warming
title_fullStr Future Atlantification of the European Arctic limited under sustained global warming
title_full_unstemmed Future Atlantification of the European Arctic limited under sustained global warming
title_short Future Atlantification of the European Arctic limited under sustained global warming
title_sort future atlantification of the european arctic limited under sustained global warming
url https://doi.org/10.1038/s41598-025-16161-8
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