Atlantic circulation acts as the planet's heat valve
Ice-age records and three climate models converge on the same result: when the AMOC weakens, the North Atlantic stops venting heat to the atmosphere and the global ocean gains it. That is a net addition, not the hemispheric redistribution the textbook seesaw predicts.
- Published in Nature Geoscience by Christo Buizert's group at Oregon State
- Past AMOC weakening warmed like 25 ppm of CO2 — about a decade of emissions
- Evidence is glacial Dansgaard-Oeschger events, not a modern-day projection