Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2

Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2

<p>The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period in which the atmospheric CO<span class="inline-formula"><sub>2</sub></span> concentration was approximately equal to the concentration we measure today (ca. 400 ppm). Sea sur...

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Main Authors: J. E. Weiffenbach, M. L. J. Baatsen, H. A. Dijkstra, A. S. von der Heydt, A. Abe-Ouchi, E. C. Brady, W.-L. Chan, D. Chandan, M. A. Chandler, C. Contoux, R. Feng, C. Guo, Z. Han, A. M. Haywood, Q. Li, X. Li, G. Lohmann, D. J. Lunt, K. H. Nisancioglu, B. L. Otto-Bliesner, W. R. Peltier, G. Ramstein, L. E. Sohl, C. Stepanek, N. Tan, J. C. Tindall, C. J. R. Williams, Q. Zhang, Z. Zhang
Format: Article
Language:English
Published: Copernicus Publications 2023-01-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/19/61/2023/cp-19-61-2023.pdf

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https://cp.copernicus.org/articles/19/61/2023/cp-19-61-2023.pdf

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