Deep-water circulation changes lead North Atlantic climate during deglaciation

Constraining the response time of the climate system to changes in North Atlantic Deep Water (NADW) formation is fundamental to improving climate and Atlantic Meridional Overturning Circulation predictability. Here we report a new synchronization of terrestrial, marine, and ice-core records, which a...

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Detalles Bibliográficos
Publicado en:Nat Commun
Main Authors: Muschitiello, Francesco, D’Andrea, William J., Schmittner, Andreas, Heaton, Timothy J., Balascio, Nicholas L., deRoberts, Nicole, Caffee, Marc W., Woodruff, Thomas E., Welten, Kees C., Skinner, Luke C., Simon, Margit H., Dokken, Trond M.
Formato: Artigo
Idioma:Inglês
Publicado: Nature Publishing Group UK 2019
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Article
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC6426850/
https://ncbi.nlm.nih.gov/pubmed/30894523
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-09237-3
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