Arctic and Antarctic forcing of ocean interior warming during the last deglaciation

• Published in: Scientific Reports
• Main Authors: Stewart, Joseph A., Robinson, Laura F., Rae, James W. B., Burke, Andrea, Chen, Tianyu, Li, Tao, de Carvalho Ferreira, Maria Luiza, Fornari, Daniel J.
• Other Authors: NERC, University of St Andrews. School of Earth & Environmental Sciences, University of St Andrews. Centre for Energy Ethics, University of St Andrews. St Andrews Isotope Geochemistry
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2024
• Subjects: GE Environmental Sciences; DAS; GE; Arctic; Antarctic; Southern Ocean; Pacific; Antarc*
• Online Access: http://hdl.handle.net/10023/29054; https://doi.org/10.1038/s41598-023-49435-0

Funding was provided by an Antarctic Bursary awarded to J.A.S., ERC and NERC grants awarded to L.F.R. (278705, NE/S001743/1, NE/R005117/1) and L.F.R. and J.W.B.R. (NE/N003861/1). Subsurface water masses formed at high latitudes impact the latitudinal distribution of heat in the ocean. Yet uncertainty surrounding the timing of low-latitude warming during the last deglaciation (18–10 ka) means that controls on sub-surface temperature rise remain unclear. Here we present seawater temperature records on a precise common age-scale from East Equatorial Pacific (EEP), Equatorial Atlantic, and Southern Ocean intermediate waters using new Li/Mg records from cold water corals. We find coeval warming in the tropical EEP and Atlantic during Heinrich Stadial 1 (+ 6 °C) that closely resemble warming recorded in Antarctic ice cores, with more modest warming of the Southern Ocean (+ 3 °C). The magnitude and depth of low-latitude ocean warming implies that downward accumulation of heat following Atlantic Meridional Overturning Circulation (AMOC) slowdown played a key role in heating the ocean interior, with heat advection from southern-sourced intermediate waters playing an additional role. Publisher PDF Peer reviewed