Its collapse would have dire consequences for our weather and life on Earth.
The Atlantic Meridional Overturning Circulation (AMOC) — which the Gulf Stream is a major part of — helps maintain the energy balance in the Atlantic Ocean. It is often described as a “conveyor belt” that takes warm surface water from the tropics and distributes it to the north Atlantic. The colder, saltier water then sinks and flows south.
Global weather patterns are critically linked to the circulation and its transport of heat and nutrients around the planet. A collapse of this system would result in significant and abrupt changes, including fast sea level rise, more extreme winters in Western Europe and disruptions to monsoon systems in the tropics.
It could also have a cascading effect and destabilize other components of the Earth’s climate system, including the Antarctic ice sheet and the Amazon rainforest.
This scenario was the premise for the 2004 climate science fiction film “The Day After Tomorrow,” in which a series of extreme weather disasters strike after climate change caused the AMOC to collapse.
The circulation is weaker than it has been in around 1,000 years, scientists had previously said, but they did not know whether it had actually been destabilized or undergoing natural changes. This week’s study used eight datasets looking at surface temperatures and salinity in the North Atlantic over a period of 150 years, and found global warming was driving the destabilization.
“The difference is crucial,” the study’s author, Niklas Boers from the Potsdam Institute for Climate Impact Research, told CNN in an email.
“Imagine a chair, which can be either shifted (with all four legs remaining on the ground) or tilted. Both change the position of the chair (corresponding to the change in mean AMOC strength), but in the first case the stability of the chair won’t be affected, while in the latter case there exists a critical point. If we tilt the chair just slightly further, it will fall down. My results suggest that what is happening to the AMOC is more likely to be a tilting than only a shifting, so the AMOC has moved toward the critical threshold at which it may collapse,” he said.
Boers added that he himself was surprised by his findings that the AMOC had been destabilized and was “moving toward its critical threshold, at which it could abruptly collapse.”
A collapse of the circulation would mean significant cooling in Europe, Beors said, “but maybe more concerning is the effect of an AMOC collapse on the tropical monsoon systems of South America, Western Africa, and India; especially in Western Africa, an AMOC collapse could lead to permanent drought conditions.”
Boers recognizes in his study that he and other scientists still don’t know if and when the current might collapse, but he called on the world to reduce greenhouse gas emissions “as much and as quickly as possible.”
“Every gram of extra greenhouse gas in the atmosphere will increase to the probability of an AMOC collapse in the future, so emitting as little as possible, both on individual but of course also on collective and international level, is the key.”