Quantifying risk of a noise-induced AMOC collapse from northern and tropical Atlantic Ocean variability
R. Chapman (1), P. Ashwin (1), J. Baker (2), R. A. Wood (2) ((1), University of Exeter, Exeter, UK, (2) Met Office Hadley Centre, Exeter, UK)

TL;DR
This study assesses how internal Atlantic Ocean variability influences the risk of noise-induced AMOC collapse, emphasizing the importance of accurately modeling decadal variability for reliable climate projections.
Contribution
It demonstrates that current models underestimate Atlantic variability, which significantly impacts the likelihood of AMOC collapse under natural fluctuations and external forcing.
Findings
Noise-induced collapse is unlikely without external forcing shifts.
Current models underestimate Atlantic variability, increasing collapse risk.
Forcing can temporarily overshoot thresholds, affecting collapse probability.
Abstract
The Atlantic Meridional Overturning Circulation (AMOC) exerts a major influence on global climate. There is much debate about whether the current strong AMOC may collapse as a result of anthropogenic forcing and/or internal variability. Increasing the noise in simple salt-advection models can change the apparent AMOC tipping threshold. However, it's not clear if 'present-day' variability is strong enough to induce a collapse. Here, we investigate how internal variability affects the likelihood of AMOC collapse. We examine internal variability of basin-scale salinities and temperatures in four CMIP6 pre-industrial simulations. We fit this to an empirical, process-based AMOC box model, and find that noise-induced AMOC collapse (defined as a decade in which the mean AMOC strength falls below 5 Sv) is unlikely for pre-industrial CMIP6 variability unless external forcing shifts the AMOC…
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