Chaotic Intrinsic Variability in the Arctic‐North Atlantic Ocean and Its Link to Sea Ice

Abstract We provide the first quantification of chaotic intrinsic variability (CIV) in the Arctic‐North Atlantic region, using an ensemble of 13 eddy‐permitting ocean–sea ice simulations. By isolating oceanic CIV from atmospheric variability, we show that CIV contributes 20%–60% of sea surface temperature interannual variability in the northern North Atlantic at the Arctic gateways, with a greater influence at subsurface levels. Salinity CIV accounts for 20%–50% of interannual variability, particularly in the Arctic. Furthermore, CIV contributes to a notable portion of sea ice concentration interannual variability in the marginal ice zone, likely influenced by dynamical interactions between sea ice and small‐scale features. CIV is shown to emerge in preferential regions, with its seasonal amplitude modulated by sea ice conditions. Given the potential for CIV to amplify in a warming Arctic, understanding its role in ocean and sea ice variability under changing climate conditions is crucial for improving predictions in this region.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-05-30
DOI
https://doi.org/10.1029/2024gl113318
Citations
1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.30
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article

Chaotic Intrinsic Variability in the Arctic‐North Atlantic Ocean and Its Link to Sea Ice

Claude Talandier, Éric Maisonnave, Camille Lique, Rym Msadek et al.
1 citations
Geophysical Research Letters
Arctic and Antarctic ice dynamics
1.30
article

Chaotic Intrinsic Variability in the Arctic‐North Atlantic Ocean and Its Link to Sea Ice

Claude Talandier, Éric Maisonnave, Camille Lique, Rym Msadek, Thierry Penduff, Camille Le Gloannec
article en
1 citations

Abstract

Abstract We provide the first quantification of chaotic intrinsic variability (CIV) in the Arctic‐North Atlantic region, using an ensemble of 13 eddy‐permitting ocean–sea ice simulations. By isolating oceanic CIV from atmospheric variability, we show that CIV contributes 20%–60% of sea surface temperature interannual variability in the northern North Atlantic at the Arctic gateways, with a greater influence at subsurface levels. Salinity CIV accounts for 20%–50% of interannual variability, particularly in the Arctic. Furthermore, CIV contributes to a notable portion of sea ice concentration interannual variability in the marginal ice zone, likely influenced by dynamical interactions between sea ice and small‐scale features. CIV is shown to emerge in preferential regions, with its seasonal amplitude modulated by sea ice conditions. Given the potential for CIV to amplify in a warming Arctic, understanding its role in ocean and sea ice variability under changing climate conditions is crucial for improving predictions in this region.

Geophysical Research LettersVol. 52(11)
Institut polytechnique de Grenoble (FR), Centre National de la Recherche Scientifique (FR), Ifremer (FR), Université de Bretagne Occidentale (FR), Université Fédérale de Toulouse Midi-Pyrénées (FR), Sorbonne Université (FR), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (FR), Institut des Géosciences de l'Environnement (FR), Laboratory for Ocean Physics and Satellite Remote Sensing (FR), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (FR), Institut Universitaire Européen de la Mer (FR), Institut de Recherche pour le Développement (FR), Université Grenoble Alpes (FR)
Life below water
Openalex Percentile: Top 22%
Arctic and Antarctic ice dynamics
1.30
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