The North Atlantic 'cold blob' could reshape Europe’s weather, scientists warn
Ongoing heatwaves are shadowed by a large cool patch in the North Atlantic known as the “cold blob,” which scientists think may signal changes in the Atlantic Meridional Overturning Circulation (AMOC). Fresh Greenland meltwater and altered heat exchange could slow the sinking of warm water, weakening AMOC and nudging the jet stream, potentially bringing more European heatwaves in the near term while raising the possibility of colder European conditions if the current weakens further. The science is still debated on exact causes and timing, but climate models generally project some AMOC weakening this century, underscoring the need to cut greenhouse gas emissions to mitigate risk.
