Internal variability effect doped by climate change drove the 2023 marine heat extreme in the North Atlantic
Year: 2025
Type: article
Abstract: The year 2023 shattered numerous heat records globally and regionally. We here focus on the origins of the unprecedented and persistent warm sea surface temperature (SST) anomalies in the North Atlantic Ocean. Using a combination of multiple observational datasets and climate model large ensemble outputs, we show that the 2023 North Atlantic SST event is a manifestation of anthropogenically-forced warming, exacerbated by an extreme phase of internal climate variability and associated regional surface flux anomalies. The long-term stratification increase due to anthropogenically-driven ocean warming amplified the impacts of internal variability. At current global warming level, the 2023 event is assessed as a decadal-type occurrence for SST anomalies averaged across the entire North Atlantic basin, but it is estimated as a centennial-type event for the subtropics and the eastern basin. The distinctive horseshoe-shaped regional distribution of these anomalies is crucial to consider for correct communication and risk assessment in a warming climate.
Institutions: Centre National de la Recherche Scientifique, Centre National de Recherches Météorologiques, Météo-France, Université de Toulouse, Université Paris Sciences et Lettres, École Normale Supérieure - PSL, Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique, Climat, Environnement, Couplages et Incertitudes, Sorbonne Université, Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, Institut de Recherche pour le Développement, Université Toulouse III - Paul Sabatier, Institut de Mécanique des Fluides de Toulouse
Language: English
Subfield: Global and Planetary Change
Field: Environmental Science
Domain: Physical Sciences
SDG: Climate action
Open Access status: gold
Estimated APC paid: $3,490
OpenAlex ID: W4409498007
