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Ocean Currents Slowing: Global Weather Chaos Looms
11 Jun
Summary
- The Atlantic Meridional Overturning Circulation is weakening.
- A resulting cold blob may trigger extreme weather events.
- Scientists debate whether ocean or atmospheric forces cause the slowdown.

A significant slowdown in the Atlantic Meridional Overturning Circulation (AMOC), a vast system of ocean currents, is becoming increasingly evident. This phenomenon is leading to the formation of a cold mass of water near Greenland, a "cold blob" that is intensifying as global temperatures rise.
This developing cold blob has substantial implications for global weather patterns, potentially disrupting atmospheric jet streams and increasing the frequency of extreme weather events in North America and Europe. Scientists are actively researching the exact causes of the AMOC's weakening.
There is a division among researchers regarding the primary driver of this slowdown. Some experts, like Laifang Li, suggest atmospheric forces are at play, while others, such as Stefan Rahmstorf, argue that oceanic conditions, specifically heat loss from the ocean surface since 1955, are the more likely cause. The potential collapse of the AMOC is considered a climate tipping point, with predictions suggesting drastic climate shifts by 2040.