Multistability and intermediate tipping of the Atlantic Ocean circulation

Lohmann, J. ORCID: https://orcid.org/0000-0002-6323-6243, Dijkstra, H. A., Jochum, M., Lucarini, V. ORCID: https://orcid.org/0000-0001-9392-1471 and Ditlevsen, P. D. ORCID: https://orcid.org/0000-0003-2120-7732 (2024) Multistability and intermediate tipping of the Atlantic Ocean circulation. Science Advances, 10 (12). eadi4253. ISSN 2375-2548 doi: 10.1126/sciadv.adi4253

Abstract/Summary

Tipping points (TP) in climate subsystems are usually thought to occur at a well-defined, critical forcing parameter threshold, via destabilization of the system state by a single, dominant positive feedback. However, coupling to other subsystems, additional feedbacks, and spatial heterogeneity may promote further small-amplitude, abrupt reorganizations of geophysical flows at forcing levels lower than the critical threshold. Using a primitive-equation ocean model, we simulate a collapse of the Atlantic Meridional Overturning Circulation (AMOC) due to increasing glacial melt. Considerably before the collapse, various abrupt, qualitative changes in AMOC variability occur. These intermediate tipping points (ITP) are transitions between multiple stable circulation states. Using 2.75 million years of model simulations, we uncover a very rugged stability landscape featuring parameter regions of up to nine coexisting stable states. The path to an AMOC collapse via a sequence of ITPs depends on the rate of change of the meltwater input. This challenges our ability to predict and define safe limits for TPs.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/115912
Identification Number/DOI	10.1126/sciadv.adi4253
Refereed	Yes
Divisions	Interdisciplinary Research Centres (IDRCs) > Centre for the Mathematics of Planet Earth (CMPE)
Uncontrolled Keywords	Multidisciplinary
Publisher	American Association for the Advancement of Science
Download/View statistics	View download statistics for this item