{
  "abstract": "The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the Earth’s climate system, and has been suggested to have multiple stable states. Critical slowing down (CSD) can detect stability changes in Earth system components, and has been found in sea-surface temperature (SST) based fingerprints of the AMOC. Here, we look for CSD in historical simulations from 27 models from the sixth Climate Model Intercomparison Project (CMIP6). We calculate three different CSD indicators for the AMOC streamfunction strengths at 26.5°N and 35°N, as well as for a previously suggested SST-based AMOC index (ASSTI) based on averaging SSTs in the subpolar gyre region. No model shows CSD in the ASSTI, which is in marked disagreement with observations. This lack of CSD is reflected in the AMOC streamfunctions in most models, although individual ensemble members in some models do show signs of CSD even under a conservative significance calculation. We thus conclude that: 1) The historical AMOC in CMIP6 models is not losing stability, 2) studies of AMOC stability should consider an ensemble of realisations, 3) there is no non-AMOC-related physical process in CMIP6 models which could cause signs of CSD in North-Atlantic SSTs in the 1850–2014 period, and thus the CSD in the observed ASSTI is likely a sign of a change in the AMOC. This final result suggests that observed changes in the ASSTI could indicate a loss of stability in the real-world AMOC.",
  "abstract_shown": true,
  "affiliations": [
    "Complexity Science, Potsdam Institute for Climate Impact Research, Potsdam, Brandenburg, Germany",
    "Munich Climate Center and Earth System Modelling Group, Department of Aerospace and Geodesy, TUM School of Engineering and Design, Technical University of Munich, Ottobrunn, Bavaria, Germany",
    "Department of Mathematics and Global Systems Institute, University of Exeter, Exeter, United Kingdom"
  ],
  "article_type": "Research Article",
  "arxiv": null,
  "author_total": 4,
  "authors": [
    {
      "affs": [
        0
      ],
      "name": "Maya Ben-Yami"
    },
    {
      "affs": [
        1
      ],
      "name": "Lana Blaschke"
    },
    {
      "affs": [
        2
      ],
      "name": "Sebastian Bathiany"
    },
    {
      "name": "Niklas Boers"
    }
  ],
  "bibtex": "https://research.draconitic.com/paper/2sx0ra7q2p5cb.bib",
  "cited_by": 2,
  "doi": "10.1371/journal.pclm.0000781",
  "fulltext_url": "https://journals.plos.org/climate/article?id=10.1371/journal.pclm.0000781",
  "id": "2sx0ra7q2p5cb",
  "issns": [
    "2767-3200"
  ],
  "landing_url": "https://journals.plos.org/climate/article?id=10.1371/journal.pclm.0000781",
  "language": null,
  "licence": "CC-BY-4.0",
  "licence_label": "CC BY 4.0",
  "licence_source": "journal",
  "licence_url": "https://creativecommons.org/licenses/by/4.0/",
  "metadata_licence": null,
  "native_subjects": [
    [
      "openalex",
      "2306|Climate variability and models"
    ],
    [
      "plos",
      "/Biology and life sciences/Paleontology/Paleoclimatology"
    ],
    [
      "plos",
      "/Computer and information sciences/Systems science/System stability"
    ],
    [
      "plos",
      "/Earth sciences/Atmospheric science/Climatology/Climate change"
    ],
    [
      "plos",
      "/Earth sciences/Atmospheric science/Climatology/Climate modeling"
    ],
    [
      "plos",
      "/Earth sciences/Atmospheric science/Climatology/Paleoclimatology"
    ],
    [
      "plos",
      "/Earth sciences/Geography/Cartography/Latitude"
    ],
    [
      "plos",
      "/Earth sciences/Marine and aquatic sciences/Bodies of water/Oceans"
    ],
    [
      "plos",
      "/Earth sciences/Paleontology/Paleoclimatology"
    ],
    [
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      "/Engineering and technology/Signal processing/Autocorrelation"
    ],
    [
      "plos",
      "/Physical sciences/Mathematics/Statistics/Statistical methods/Autocorrelation"
    ],
    [
      "plos",
      "/Physical sciences/Mathematics/Systems science/System stability"
    ],
    [
      "plos",
      "/Research and analysis methods/Mathematical and statistical techniques/Statistical methods/Autocorrelation"
    ],
    [
      "plos",
      "/Research and analysis methods/Simulation and modeling"
    ],
    [
      "plos",
      "/Research and analysis methods/Simulation and modeling/Climate modeling"
    ]
  ],
  "openalex": "W7220861451",
  "pdf_url": "https://journals.plos.org/climate/article/file?id=10.1371/journal.pclm.0000781&type=printable",
  "pmcid": null,
  "pmid": null,
  "published": "2026-10-07",
  "publisher": "Public Library of Science",
  "ris": "https://research.draconitic.com/paper/2sx0ra7q2p5cb.ris",
  "sources": [
    {
      "first_seen": "2026-10-30T12:17:30Z",
      "native_id": "10.1371/journal.pclm.0000781",
      "source": "plos",
      "url": "https://journals.plos.org/climate/article?id=10.1371/journal.pclm.0000781"
    }
  ],
  "subjects": [
    {
      "field": "biology",
      "origin": "plos:paleontology",
      "subfield": "evolutionary-biology"
    },
    {
      "field": "earth",
      "origin": "plos:climate change",
      "subfield": "climate"
    },
    {
      "field": "mathematics",
      "origin": "plos:statistical methods",
      "subfield": "statistics"
    }
  ],
  "title": "No critical slowing down in the Atlantic Overturning Circulation in historical CMIP6 simulations",
  "title_text": "No critical slowing down in the Atlantic Overturning Circulation in historical CMIP6 simulations",
  "type": "peer-reviewed",
  "updated_at": "2026-10-30T12:17:30Z",
  "url": "https://research.draconitic.com/paper/2sx0ra7q2p5cb",
  "venue": "PLOS Climate",
  "versions": []
}