The Atlantic Ocean current, of which the Gulf Stream is a part, appears to be far less stable than previously thought. A weakening of the Gulf Stream could make Europe an outlier in a warming world, experiencing slower warming or even cooling, especially during winter, while the rest of the planet heats up. A new study explores how temperature extremes in Europe might change under such conditions.
Recent research suggests the Atlantic Meridional Overturning Circulation (AMOC), which includes the Gulf Stream, is more sensitive than previously believed. Increased precipitation and melting ice from Greenland are making North Atlantic waters less salty and dense, weakening the AMOC. This could lead to colder winters in Europe, with sea ice expanding southward and reflecting more sunlight, further cooling the region.
A study by Utrecht University and KNMI modeled various scenarios, showing that under moderate emissions (RCP4.5), winter temperatures in the Netherlands could drop by 15°C in extreme cases. However, under high emissions (RCP8.5), the impact on European temperatures might be less severe due to warmer ocean waters limiting sea ice expansion.
The study highlights the potential for increased temperature contrasts between Northern and Southern Europe, stronger storms, and more variable daily temperatures. It also warns of reduced rainfall and faster sea-level rise in the North Atlantic.
While the study provides initial insights, further research is needed to confirm the likelihood of AMOC collapse and its full climatic effects. For interactive results, visit amocscenarios.org.
