Atlantic Meridional Overturning…Atlantic Meridional Overturning CirculationCoverage from The Conversation, ScienceAlert, and others
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The Atlantic Meridional Overturning Circulation, or AMOC, is a large-scale ocean system that carries warm water northward, where cooling and sinking help drive a return flow through the Atlantic.
Research examines whether ocean warming and freshwater from Greenland’s melting ice are weakening this circulation and increasing the risk of a tipping point or eventual shutdown. Observations, climate models, and statistical warning indicators inform estimates of that risk, though the timing and magnitude remain uncertain. A major weakening could affect European temperatures, rainfall belts, regional sea levels, carbon exchange, and climate patterns across the Arctic, Atlantic, and Southern Ocean.
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Researchers used Nova Scotia seabed sediments to reconstruct Younger Dryas ocean changes and found Gulf Stream-driven warming consistent with AMOC weakening mechanisms.
Researchers led by Christo Buizert reported in Nature Geoscience that Pleistocene AMOC changes regulated planetary heat storage through North Atlantic convection, with implications for future weakening.
Scientists report that a persistent cold North Atlantic anomaly near Iceland and Greenland may signal AMOC weakening and contribute to longer European heat waves.
Nature-published research projects Atlantic Meridional Overturning Circulation weakening up to 50% by 2100, potentially shifting storms, rainfall, and coastal risk.
4/22/2026 • Climate Science & Impacts • General
Is a deep freeze coming? - Prospect Magazine / Ellen Halliday83
Stefan Rahmstorf and Tim Lenton describe rising AMOC tipping-point risk for climate under warming, with the UK lacking explicit adaptation plans while Iceland treats AMOC as national security.
Scientists report human-driven weakening of AMOC in the North Atlantic, using RAPID, OSNAP, and SAMBA observations, with uncertain timing of any major transition.
Climate researchers, including Christo Buizert, describe evidence of past abrupt AMOC-related shifts and uncertain projected weakening this century in the North Atlantic.
An international research team reported in 2026 that late Pliocene AMOC strengthened despite near cessation of Agulhas Leakage near South Africa around 3.4 million years ago.
Nature Communications published a University of California, Riverside study projecting AMOC slowing to intensify California atmospheric rivers and reduce Greenland snowfall under high emissions.
Scientists use Argo floats and paleoclimate evidence to study AMOC weakening risks, including potential abrupt regional weather impacts across the North Atlantic and UK.
Stefan Rahmstorf-led findings connect North Atlantic cooling since 1900 to ocean heat transport and possible AMOC weakening with future European climate risks.
Tim Lenton and researchers model Atlantic Meridional Overturning Circulation collapse risk, projecting at least a 10 percent chance affecting northern Europe.
Researchers using 21 climate simulations estimate a 10 to 23 percent chance that AMOC collapse in the North Atlantic may already be committed, depending on emissions timing and Greenland ice melt.
Researchers analyzing North Atlantic heat fluxes since 1870 report Greenland-adjacent cooling, suggesting possible AMOC instability and downstream rainfall and storm impacts.
European and US agencies face proposed funding cuts to AMOC monitoring, despite projected weakening that could affect European weather and sea-level rise.
Eight climate models project stronger mid-century AMOC weakening when Europe and North America cut aerosol emissions without concurrent decarbonisation.
Researchers warn AMOC weakening could approach tipping risk, with uncertain timing and potential climate impacts for Europe, Africa, Asia, and the Southern Ocean.
Scientists warn the Atlantic meridional overturning circulation could be nearing collapse, potentially driving abrupt cooling, storms, and faster sea-level rise in coming years.
Researchers estimate AMOC could weaken 43% to 59% by 2100, using bias-corrected Atlantic observations, while scientists stress major uncertainty in tipping-point risk.
Climate modelers project AMOC shutdown could release up to 640 billion tonnes of CO2 near Antarctica and likely become irreversible at current CO2 levels.
Researchers reported in Science Advances on April 29 that volcanic eruptions likely disrupted AMOC during the Younger Dryas, showing high ocean-circulation sensitivity to disturbances.
Idaho State University researchers report that North Atlantic circulation disruption near Greenland cooled Alaska mainly in winter about 13,000 years ago, based on lake sediments and Greenland ice cores.
Chuncheng Guo and colleagues found in a climate-model simulation that the AMOC could strengthen within decades after global cooling, though the scenario requires enormous carbon removal worldwide.
A Nature Geoscience modeling study led by Christo Buizert at Oregon State University found that weakening Atlantic circulation could cool northern Europe while increasing global warming.
Stefan Rahmstorf and colleagues report long-term cooling southeast of Greenland consistent with AMOC weakening using observation-based climate reanalyses.
Researchers proposed a Bering Strait dam in Science Advances to stabilize AMOC by reducing Pacific freshwater inflow, while the UK Met Office cautioned against geoengineering risks.
Jelle Soons and Henk Dijkstra presented Bering Strait dam simulations at the European Geosciences Union meeting in Vienna on 5 May, finding potential AMOC strengthening under early construction.
Researchers using extended IPCC model runs report the AMOC tipping point may be reached within decades, increasing shutdown risk for the North Atlantic and Europe.
Utrecht University researchers reported in Nature Climate Change that rapid warming could cause Atlantic circulation collapse near 2°C, affecting Europe and other regions.
Andrew Watson and Phil Williamson dispute AMOC collapse claims in responses, citing projections for higher odds of 50 percent weakening by late-century under continued fossil-fuel emissions.
Scientists project AMOC slowdown by 2100, warning of regional climate impacts while political climate responses are described as misaligned with risk scale.
4/17/2026 • Policy, Politics & Governance • General