Preprints
https://doi.org/10.5194/egusphere-2026-1872
https://doi.org/10.5194/egusphere-2026-1872
10 Apr 2026
 | 10 Apr 2026
Status: this preprint is open for discussion and under review for Nonlinear Processes in Geophysics (NPG).

Predicting the distance of the AMOC to its tipping point using CNNs

Francesco Guardamagna, Sacha Sinet, and Henk A. Dijkstra

Abstract. The Atlantic Meridional Overturning Circulation (AMOC) is an important tipping element of the climate system, with the potential to undergo an abrupt transition from its present strong state to a weak state. Such a collapse would have severe global consequences, including regional cooling, sea-level rise, altered precipitation patterns, and cascading impacts on other climate tipping elements. Both statistical and physics-based early warning signals (EWS) of an approaching AMOC tipping event have been proposed. Here, we introduce a convolutional neural network (CNN)–based framework designed to predict the distance of an AMOC state to its tipping point under imposed freshwater flux forcing. We first evaluate the CNN model using simulations from the Earth System Model of Intermediate Complexity CLIMBER-X. We then test its generalization capabilities by applying the CNN model, trained on CLIMBER-X data, to the AMOC tipping trajectory obtained recently in the Community Earth System Model (CESM). Explainable AI methods are used to identify the spatiotemporal features most relevant to the predictions. Our results demonstrate the potential of deep learning to provide reliable estimates of the distance to the AMOC tipping point and generalize across models of varying complexity.

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Francesco Guardamagna, Sacha Sinet, and Henk A. Dijkstra

Status: open (until 05 Jun 2026)

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Francesco Guardamagna, Sacha Sinet, and Henk A. Dijkstra

Model code and software

Code for reproducing the results of the paper "Predicting the Distance of the AMOC to Its Tipping Point Using CNNs" Francesco Guardamagna https://doi.org/10.5281/zenodo.19369578

Francesco Guardamagna, Sacha Sinet, and Henk A. Dijkstra
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Latest update: 11 Apr 2026
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Short summary
The Atlantic Meridional Overturning Circulation (AMOC) is an ocean current that redistributes heat in the Atlantic Ocean and may abruptly weaken under climate change, with impacts including cooling in Europe and sea-level rise along the North American East Coast. Freshwater input from melting ice into the North Atlantic can push the system toward a tipping point. We introduce an artificial intelligence-based method to estimate the distance to this tipping point in terms of freshwater forcing.
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