Annually resolved Atlantic sea surface temperature variability over the past 2,900 y.


Journal

Proceedings of the National Academy of Sciences of the United States of America
ISSN: 1091-6490
Titre abrégé: Proc Natl Acad Sci U S A
Pays: United States
ID NLM: 7505876

Informations de publication

Date de publication:
03 11 2020
Historique:
pubmed: 14 10 2020
medline: 5 1 2021
entrez: 13 10 2020
Statut: ppublish

Résumé

Global warming due to anthropogenic factors can be amplified or dampened by natural climate oscillations, especially those involving sea surface temperatures (SSTs) in the North Atlantic which vary on a multidecadal scale (Atlantic multidecadal variability, AMV). Because the instrumental record of AMV is short, long-term behavior of AMV is unknown, but climatic teleconnections to regions beyond the North Atlantic offer the prospect of reconstructing AMV from high-resolution records elsewhere. Annually resolved titanium from an annually laminated sedimentary record from Ellesmere Island, Canada, shows that the record is strongly influenced by AMV via atmospheric circulation anomalies. Significant correlations between this High-Arctic proxy and other highly resolved Atlantic SST proxies demonstrate that it shares the multidecadal variability seen in the Atlantic. Our record provides a reconstruction of AMV for the past ∼3 millennia at an unprecedented time resolution, indicating North Atlantic SSTs were coldest from ∼1400-1800 CE, while current SSTs are the warmest in the past ∼2,900 y.

Identifiants

pubmed: 33046633
pii: 2014166117
doi: 10.1073/pnas.2014166117
pmc: PMC7959532
doi:

Types de publication

Historical Article Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S.

Langues

eng

Sous-ensembles de citation

IM

Pagination

27171-27178

Informations de copyright

Copyright © 2020 the Author(s). Published by PNAS.

Déclaration de conflit d'intérêts

The authors declare no competing interest.

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Auteurs

Francois Lapointe (F)

Climate System Research Center, Department of Geosciences, University of Massachusetts, Amherst, MA 01003; flapointe@umass.edu.
Centre-Eau Terre Environnement, Institut National de la Recherche Scientifique, Université du Québec, Québec, QC G1K 9A9, Canada.

Raymond S Bradley (RS)

Climate System Research Center, Department of Geosciences, University of Massachusetts, Amherst, MA 01003.

Pierre Francus (P)

Centre-Eau Terre Environnement, Institut National de la Recherche Scientifique, Université du Québec, Québec, QC G1K 9A9, Canada.
Centre de Recherche sur la Dynamique du Système Terre (GEOTOP), Montreal, QC H3C 3P8, Canada.

Nicholas L Balascio (NL)

Department of Geology, College of William and Mary, Williamsburg, VA 23187.

Mark B Abbott (MB)

Department of Geology and Environmental Science, University of Pittsburgh, Pittsburgh, PA 15260.

Joseph S Stoner (JS)

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331.

Guillaume St-Onge (G)

Institut des sciences de la mer de Rimouski (ISMER), Université du Québec à Rimouski, Rimouski, QC G5L 3A1, Canada.

Arnaud De Coninck (A)

Centre-Eau Terre Environnement, Institut National de la Recherche Scientifique, Université du Québec, Québec, QC G1K 9A9, Canada.

Thibault Labarre (T)

Centre-Eau Terre Environnement, Institut National de la Recherche Scientifique, Université du Québec, Québec, QC G1K 9A9, Canada.

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