Asynchronous Poleward Migration of the Atlantic Subtropical Gyres Over the Past 22,000 years

Abstract By exchanging huge amounts of heat between the tropics and high latitudes, subtropical gyres significantly impact Earth's energy balance. Yet, their dynamical changes during the last deglaciation remain poorly understood. Here, nine records of the planktonic foraminiferal species Globorotalia truncatulinoides , that inhabits the permanent deep thermocline of subtropical gyres, are used to explore the meridional migration of both the North and South Atlantic subtropical gyres (NASG and SASG, respectively) in the past 22,000 years. We find that both gyres migrated poleward, with the SASG migration 1,500 years earlier than the NASG. Records from the North Atlantic Ocean indicate that the NASG's northern boundary has shifted over 6°. Climate model simulations suggest that these migrations are coupled with shifts in meridional temperature gradients. The poleward migration of the Atlantic subtropical gyres was crucial for sustaining a milder modern high‐latitude climate in comparison with that of the last ice age.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-02-03
DOI
https://doi.org/10.1029/2024gl111497
Citations
5
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
6.50

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article

Asynchronous Poleward Migration of the Atlantic Subtropical Gyres Over the Past 22,000 years

Janne Repschläger, Tainã M. L. Pinho, Stefan Mulitza, Cristiano Mazur Chiessi et al.
5 citations
Geophysical Research Letters
Geology and Paleoclimatology Research
6.50
article

Asynchronous Poleward Migration of the Atlantic Subtropical Gyres Over the Past 22,000 years

Janne Repschläger, Tainã M. L. Pinho, Stefan Mulitza, Cristiano Mazur Chiessi, André Bahr, Hu Yang, Rodrigo Costa Portilho-Ramos, Dirk Nürnberg, Gerrit Lohmann, Ralf Tiedemann, Xiaoxu Shi
article en
5 citations

Abstract

Abstract By exchanging huge amounts of heat between the tropics and high latitudes, subtropical gyres significantly impact Earth's energy balance. Yet, their dynamical changes during the last deglaciation remain poorly understood. Here, nine records of the planktonic foraminiferal species Globorotalia truncatulinoides , that inhabits the permanent deep thermocline of subtropical gyres, are used to explore the meridional migration of both the North and South Atlantic subtropical gyres (NASG and SASG, respectively) in the past 22,000 years. We find that both gyres migrated poleward, with the SASG migration 1,500 years earlier than the NASG. Records from the North Atlantic Ocean indicate that the NASG's northern boundary has shifted over 6°. Climate model simulations suggest that these migrations are coupled with shifts in meridional temperature gradients. The poleward migration of the Atlantic subtropical gyres was crucial for sustaining a milder modern high‐latitude climate in comparison with that of the last ice age.

Geophysical Research LettersVol. 52(3)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Universidade de São Paulo (BR), University of Bremen (DE), Heidelberg University (DE), GEOMAR Helmholtz Centre for Ocean Research Kiel (DE), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Max Planck Institute for Chemistry (DE), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN)
Fundação de Amparo à Pesquisa do Estado de São Paulo, National Natural Science Foundation of China, Conselho Nacional de Desenvolvimento Científico e Tecnológico
Openalex Percentile: Top 4%
Geology and Paleoclimatology Research
6.50
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