Disentangled Fingerprints suggest no historical weakening of Atlantic Overturning and Subpolar Gyre
Abstract
The AMOC and the Subpolar Gyre are key components of the Earth's climate system, both potentially prone to destabilization and abrupt shifts under anthropogenic forcing.Given the strong influence of the AMOC and the SPG on global climate, detecting changes in their stability is of high importance, yet is hindered by the limited length of observational records.In the absence of long-term direct AMOC observations, several observation-based fingerprints of the AMOC have been proposed.However, existing fingerprints do not clearly distinguish between SPG and AMOC variability, instead reflecting an opaque mixture of dynamics from both systems.Here, we assess the performance of widely used AMOC fingerprints across CMIP6 models and compare them with statistically optimal fingerprints that we derive from sea surface temperature and salinity.We show that traditional AMOC fingerprints exhibit weak correlations with both AMOC and SPG strength.In contrast, our statistically optimal fingerprints, trained on pre-industrial control simulations, consistently outperform existing approaches across independent segments of piControl simulations and historical experiments.These fingerprints accurately reconstruct AMOC and SPG variability while minimizing overlap, enabling a clear separation between the two systems.Our results provide the first tailored observational fingerprints that robustly distinguish AMOC and SPG, demonstrating the potential of statistically optimized approaches to improve detection and attribution of changes in Atlantic circulation, including precursor signals of potential tipping behavior.Applying our approach to sea surface temperature observations, we find that our optimized fingerprints do not confirm the substantial AMOC weakening in the recent decades as suggested by traditional fingerprints, but also do not rule out a loss of stability.
Related
- Cascading impacts of Atlantic meridional overturning circulation weakening and collapse on marine biogeochemistry
- No critical slowing down in the Atlantic Overturning Circulation in historical CMIP6 simulations
- Reversible Atlantic overturning despite continued Greenland ice sheet melt
- Global stability of the Atlantic overturning circulation: edge state, long transients and boundary crisis under CO2 forcing
- Centennial-scale intensifications of the Atlantic Meridional Overturning Circulation during Heinrich Stadial 1
BibTeX
@misc{emirzade2026disentangled,
title = {{Disentangled Fingerprints suggest no historical weakening of Atlantic Overturning and Subpolar Gyre}},
author = {Bahar Emirzade and Jade Ajagun-Brauns and Maya Ben-Yami and Sebastian Bathiany and Yechul Shin and Jong-Seong Kug and Niklas Boers},
howpublished = {arXiv},
year = {2026},
month = sep,
doi = {10.48550/arxiv.2609.18551},
eprint = {2609.18551},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2609.18551},
note = {CC BY 4.0},
}
RIS
TY - UNPB
TI - Disentangled Fingerprints suggest no historical weakening of Atlantic Overturning and Subpolar Gyre
AU - Bahar Emirzade
AU - Jade Ajagun-Brauns
AU - Maya Ben-Yami
AU - Sebastian Bathiany
AU - Yechul Shin
AU - Jong-Seong Kug
AU - Niklas Boers
PY - 2026
DA - 2026/09/16
PB - arXiv
DO - 10.48550/arxiv.2609.18551
UR - https://arxiv.org/abs/2609.18551
AB - The AMOC and the Subpolar Gyre are key components of the Earth's climate system, both potentially prone to destabilization and abrupt shifts under anthropogenic forcing.Given the strong influence of the AMOC and the SPG on global climate, detecting changes in their stability is of high importance, yet is hindered by the limited length of observational records.In the absence of long-term direct AMOC observations, several observation-based fingerprints of the AMOC have been proposed.However, existing fingerprints do not clearly distinguish between SPG and AMOC variability, instead reflecting an opaque mixture of dynamics from both systems.Here, we assess the performance of widely used AMOC fingerprints across CMIP6 models and compare them with statistically optimal fingerprints that we derive from sea surface temperature and salinity.We show that traditional AMOC fingerprints exhibit weak correlations with both AMOC and SPG strength.In contrast, our statistically optimal fingerprints, trained on pre-industrial control simulations, consistently outperform existing approaches across independent segments of piControl simulations and historical experiments.These fingerprints accurately reconstruct AMOC and SPG variability while minimizing overlap, enabling a clear separation between the two systems.Our results provide the first tailored observational fingerprints that robustly distinguish AMOC and SPG, demonstrating the potential of statistically optimized approaches to improve detection and attribution of changes in Atlantic circulation, including precursor signals of potential tipping behavior.Applying our approach to sea surface temperature observations, we find that our optimized fingerprints do not confirm the substantial AMOC weakening in the recent decades as suggested by traditional fingerprints, but also do not rule out a loss of stability.
ER -