The Atlantic Meridional Overturning Circulation (AMOC) is a massive ocean current system that transports warm water northward and cold water southward, regulating global climate patterns.
This oceanic conveyor belt moves approximately 15 million cubic meters of water per second—equivalent to 15 times the flow of all the world's rivers combined.
| Period | Temperature Anomaly | Context |
|---|---|---|
| 1866-05 | -0.350°C | Pre-industrial baseline |
| 1893-02 | -0.578°C | Coldest recorded month |
| 1893-05 | -0.404°C | Spring cooling period |
| 1903-05 | -0.478°C | Early 20th century |
Continued current strength
30-50% reduction in strength
Near-complete shutdown
AMOC weakening threatens major climate disruptions. Although activation does not mean immediate collapse, it marks the beginning of potentially irreversible changes to global climate systems.
“Breach of +1.5°C reference mark correlates with severe compound event escalation. Spatial, temporal, and testimonial evidence compound to narrow the safe operating space.”
Given the potential for irreversible climate system changes, continuous monitoring and risk assessment of AMOC stability is essential for climate adaptation planning.
The precautionary principle requires measuring post-tipping point consequences to overall climate system development following any activation date.