Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling
The role of Southern Ocean gateways contributing to the Eocene-Oligocene climate transition is still debated. Here, the authors present high-resolution ocean simulations to show that gateways opening led to a reorganization of ocean circulation, heat transport and Antarctic surface water cooling.
Guardado en:
Autores principales: | Isabel Sauermilch, Joanne M. Whittaker, Andreas Klocker, David R. Munday, Katharina Hochmuth, Peter K. Bijl, Joseph H. LaCasce |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2021
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Materias: | |
Acceso en línea: | https://doaj.org/article/3b7c0e4a2a9848b28a92e690b0bddeac |
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