A Key Atlantic Current Is Weakening. Here’s Why It Matters. | DW News

DW News (Deutsche Welle)
DW News (Deutsche Welle)May 5, 2026

Why It Matters

A weakening AMOC could reshape Europe’s climate, amplifying heatwaves, storms, and sea‑level rise, making swift emissions cuts essential to avoid irreversible regional impacts.

Key Takeaways

  • Europe's warming fastest, but Atlantic conveyor may soon weaken.
  • New study raises AMOC shutdown odds to 25‑70% by century.
  • Freshwater influx and surface warming prevent deep‑water sinking in North Atlantic.
  • Cooling “cold blob” already altering European pressure patterns and heat extremes.
  • Only rapid emissions cuts can lower tipping‑point risk, but reversal unlikely.

Summary

The video explains that Europe’s record‑fast warming hinges on the Atlantic Meridional Overturning Circulation (AMOC), a deep‑sea conveyor that transports warm, salty water northward. New research in Science Advances suggests the AMOC’s tipping point could arrive within decades, with shutdown probabilities rising from a historic 5% to 25% under low‑emission scenarios and up to 70% under high‑emission pathways.

Scientists attribute the slowdown to two climate‑driven forces: surface warming that makes water less dense, and an influx of fresh meltwater that dilutes salinity. Both inhibit the sinking of water in the North Atlantic, a critical step for the conveyor’s circulation. The resulting “cold blob” of cooler surface water west of Britain is already reshaping pressure systems, fostering persistent low‑pressure zones that paradoxically amplify heatwaves across Europe.

Professor Stefan Ramstov emphasizes that the observed cold blob is a tangible early warning sign, not a Hollywood fantasy. While the AMOC would not collapse overnight, its gradual weakening over 50‑100 years could trigger regional cooling in northern Europe, heightened temperature gradients, more severe storms, and an additional half‑meter of sea‑level rise on top of global trends.

The stakes are clear: without rapid decarbonisation, Europe faces a climate paradox of simultaneous warming and cooling that will intensify weather extremes and drought risk. Mitigating emissions now is the only realistic strategy to lower the probability of crossing the irreversible tipping point.

Original Description

A vast Atlantic current, the Atlantic Meridional Overturning Circulation (AMOC), shapes Europe's climate and global weather.
Professor Stefan Rahmstorf breaks down why scientists are more concerned about its stability than ever before.
00:00 The paradox at the heart of Europe's rising temperatures
00:39 Could the AMOC shut down by century's end?
02:13 The role of the predicted "cold blob"
04:41 How the AMOC conveyor belt moves heat around Europe
05:11 How global warming and glacier freshwater melt disrupt the system
07:31 Are slowdown effects already visible in Europe’s weather?
08:55 More extremes ahead: heat, cold, drought, floods and storms
11:09 Can carbon cuts stop or reverse the AMOC slowdown?
#dwcurrentaffairs #climatechange #gulfstream
For more news go to: http://www.dw.com/en/
Follow DW on social media:
Für Videos in deutscher Sprache besuchen Sie: https://www.youtube.com/dwdeutsch

Comments

Want to join the conversation?

Loading comments...