The 1600 CE Huaynaputina eruption as a possible trigger for persistent cooling in the North Atlantic region

The 1600 CE Huaynaputina eruption as a possible trigger for persistent cooling in the North Atlantic region

Paleoclimate reconstructions have identified a period of exceptional summer and winter cooling in the North Atlantic region following the eruption of the tropical volcano Huaynaputina (Peru) in 1600 CE. A previous study based on numerical climate simulations has indicated a potential mechanism for t...

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Bibliographic Details
Main Authors: Corona, C. (Author), Degroot, D. (Author), Huhtamaa, H. (Author), Moreno-Chamarro, E. (Author), Stoffel, M. (Author), White, S. (Author), Zanchettin, D. (Author)
Format: Article
Language:English
Published: Copernicus GmbH 2022
Subjects:
Atlantic Ocean
Atlantic Ocean (North)
climate conditions
cooling
gyre
paleoclimate
volcanic eruption
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