UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Early Interglacial Legacy of Deglacial Climate Instability

Barker, S; Knorr, G; Conn, S; Lordsmith, S; Newman, D; Thornalley, D; (2019) Early Interglacial Legacy of Deglacial Climate Instability. Paleoceanography and Paleoclimatology , 34 (8) pp. 1455-1475. 10.1029/2019PA003661. Green open access

[thumbnail of Thornalley_2019PA003661.pdf]
Preview
Text
Thornalley_2019PA003661.pdf

Download (5MB) | Preview

Abstract

Throughout the last glacial cycle millennial timescale variations in atmospheric CO2 occurred in parallel with perturbations in deep ocean circulation, which were themselves reflected by observable changes in surface conditions across the North Atlantic region. Here we use continuous proxy records to argue that an equivalent relationship has held throughout the last 800 kyr, that is, since before the first occurrence of Heinrich events (strictly defined). Our results highlight the importance of internal climate dynamics in amplifying external (insolation) forcing on the climate system to produce the large amplitude of glacial terminations (deglaciations) during the middle to late Pleistocene. We show that terminations are characterized by an interval of intense ice rafting followed by a subsequent and abrupt shift to anomalously warm surface conditions (with respect to the more gradually evolving background state), which we interpret to reflect an abrupt recovery of deep ocean circulation in the Atlantic. According to our synthesis, this is followed by a period of enhanced (or at least anomalous) overturning lasting thousands of years until equilibrium interglacial conditions are attained and during which atmospheric CO2 is likely to decrease. Our results therefore suggest that deglacial oscillations in ocean circulation can have a lasting influence on early interglacial climate and highlight the transient nature of atmospheric CO2 overshoots associated with the onset of some previous interglacials. Accordingly, we suggest that these intervals should be considered as a part of the deglacial process. This has implications for studies concerned with the evolution of atmospheric CO2 during interglacial periods including the Holocene.

Type: Article
Title: Early Interglacial Legacy of Deglacial Climate Instability
Open access status: An open access version is available from UCL Discovery
DOI: 10.1029/2019PA003661
Publisher version: https://doi.org/10.1029/2019PA003661
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/10081650
Downloads since deposit
127Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item