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Science Not yet confirmed elsewhere1 publisher 2 min read Published

Danish model has a weakened AMOC regaining strength within decades of cooling

Danish Meteorological Institute researchers report that the AMOC starts strengthening within decades of global cooling in one climate model. Getting that cooling at 0.2C a decade would take carbon removal equal to current annual emissions.

The Scientist · Science desk

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Illustration accompanying Danish model has a weakened AMOC regaining strength within decades of cooling
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Cooling at 0.2C a decade needs far more removal Carbon removal as a share of humanity's annual emissions: what the world removes now and what cooling at 0.2C per decade would require.

Carbon removal goes from 0.1 per cent of annual emissions today, around 2 million tonnes a year, to the 100 per cent of current annual emissions, 45 petagrams a year, needed to cool the world at 0.2C per decade.

Cooling at 0.2C a decade needs far more removal
MeasureValueAs ofClaim
Removed per year today0.1% of emissionsToday9
Needed to cool 0.2C a decade100% of emissionsRequired10

What happened

  • A collapse of the AMOC would bring "ice age" winters to Europe, higher sea levels in North America and disrupted monsoons in Africa and Asia, according to New Scientist.
  • The simulation counted melting of the Greenland ice sheet as well as higher air temperatures.
  • With warming at 0.2C per decade, slightly slower than the current rate, the AMOC weakened significantly over centuries but did not shut down entirely.
  • The world now removes around 2 million tonnes of carbon a year, equal to 0.1 per cent of annual emissions, through direct air capture and enhanced weathering.

Why it matters

  • contradiction The recovery result comes from one model that may overstate the AMOC's stability, yet a study published in July 2026 also found slowdown could be reversed by cutting atmospheric CO2.
  • decision Cooling on this scale may force a choice on solar radiation management, an option Utrecht's Rene van Westen says might be necessary.
  • exposure Europe is the region exposed to a restart: Van Westen warns of accelerated warming after a period of dramatic cooling.

Earlier tipping studies pushed the forcing one way. Chuncheng Guo of the Danish Meteorological Institute said "most of the previous studies are only looking at warming scenarios" [4]. In the cooling case, the current responded along the same line as in the warming case. "There's a very linear relationship between the global mean temperature and the AMOC response," Guo said [3].

In our view, that linearity is both the result and the open question. A response that moves in step with temperature leaves no room for the current to stay weak after the forcing reverses. A model with no sharp threshold would produce the same behaviour.

The same run also limits what "collapse" means here. Guo said the AMOC would not be totally extinguished even with up to 10C of warming [7], yet he framed the test as whether the current would "stay in that collapsed state" [4]. Because the current never fully stops in this model, the run cannot test recovery from a full shutdown [6][7]. The size of the weakening is not given.

The cooling side needs the same care with denominators. Cooling at 0.2C per decade would take 45 petagrams of carbon removal a year, which the account equates to 100 per cent of current annual emissions [10]. It puts today's removal at 0.1 per cent of emissions [9]. Those two figures imply a 1,000-fold increase [18]. But a petagram is a billion tonnes, and 45 billion tonnes set against the account's stated tonnage for current removal gives a 22,500-fold increase [17]. The two comparisons do not reconcile. Either way the scale-up is at least a thousandfold.

Guo was direct about what that means. "AMOC reversibility does not mean safety, because we really need a huge, huge amount of carbon dioxide removal to achieve that cooling rate," he said [11]. "That is not something we can achieve with today's technology," he said [11].

What to watch

  • The German rerun of the same experiment across 10 climate models. It will show whether the linear response and the recovery hold outside one model.
  • Any model run in which the AMOC stays weak after the forcing reverses. A result like that would break the near-linear picture.
  • Whether the authors publish carbon removal figures that reconcile the tonnage and the percentages.

Clarity's read

What the record supports and how the coverage leans. The claims behind it follow.

Reality

Evidence40
Adoption
Insufficient
Hype gap+10
Incentives
Insufficient
Confidence45
Why these scores

Claim ledger

Ranked by verification strength, evidence, and original report placement.

  1. [1]

    A collapse in the AMOC would be catastrophic, bringing 'ice age' winters to Europe, raising sea levels in North America and disrupting monsoons in Africa and Asia.

    Reported Supported Source: New ScientistView cited source
  2. [2]

    Guo and colleagues used a climate model to simulate the AMOC's strength as global temperatures rise with carbon emissions, and found the AMOC could weaken significantly but would recover just as quickly if global cooling occurs.

    Reported Supported Source: New Scientist, reporting Chuncheng Guo, Danish Meteorological InstituteView cited source
  3. [3]

    "There's a very linear relationship between the global mean temperature and the AMOC response," said Chuncheng Guo at the Danish Meteorological Institute.

    Reported Supported Source: Chuncheng Guo, Danish Meteorological InstituteView cited source

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Sources

1 independent publisher whose own reporting we read for this story.

  1. newscientist.com

    1 article · October 14, 2026

    We can rescue the AMOC after its collapse – but it won’t be easy

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