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Surface climate signals transmitted rapidly to deep North Atlantic throughout last millennium

Lu, Wanyi; Oppo, Delia W; Gebbie, Geoffrey; Thornalley, David JR; (2023) Surface climate signals transmitted rapidly to deep North Atlantic throughout last millennium. Science , 382 (6672) pp. 834-839. 10.1126/science.adf1646. Green open access

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Abstract

Instrumental observations of subsurface ocean warming imply that ocean heat uptake has slowed 20th-century surface warming. We present high-resolution records from subpolar North Atlantic sediments that are consistent with instrumental observations of surface and deep warming/freshening and in addition reconstruct the surface-deep relation of the last 1200 years. Sites from ~1300 meters and deeper suggest an ~0.5 degrees celsius cooling across the Medieval Climate Anomaly to Little Ice Age transition that began ~1350 ± 50 common era (CE), whereas surface records suggest asynchronous cooling onset spanning ~600 years. These data suggest that ocean circulation integrates surface variability that is transmitted rapidly to depth by the Atlantic Meridional Ocean Circulation, implying that the ocean moderated Earth’s surface temperature throughout the last millennium as it does today.

Type: Article
Title: Surface climate signals transmitted rapidly to deep North Atlantic throughout last millennium
Open access status: An open access version is available from UCL Discovery
DOI: 10.1126/science.adf1646
Publisher version: https://doi.org/10.1126/science.adf1646
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL SLASH
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS > Dept of Geography
URI: https://discovery.ucl.ac.uk/id/eprint/10181552
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