Catastrophic changes in global weather patterns could be on the horizon as scientists confirm the warming Atlantic current has reached a “new record low”.

The Gulf Stream current, which has not been running at peak strength for centuries, is now at its weakest point in the past 1,600 years.

Climate change resulting from rising levels of carbon dioxide in the atmosphere is a likely cause of this phenomenon.

The Atlantic meridional overturning circulation (Amoc), the system of currents that transports warm water from the tropics via the Gulf Stream to the North Atlantic, plays a major role in regulating the world’s climate.

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A fictional depiction of Amoc’s collapse was portrayed in The Day After Tomorrow, and while the film’s events were exaggerated, scientists say severe weather events are likely to result from the ongoing changes.

If the system continues to slow down, there could be weather disruption across the US, Europe and Africa, and sea levels could rise rapidly on the US east coast.

Two international teams of scientists have undertaken extensive analyses of sea surface temperature data and underwater sediments. Both studies were published in the journal Nature.

In both papers, the researchers found Amoc had slowed down by roughly 15 per cent, although the timescales over which this weakening had taken place were very different.

While one study found the dip had occurred over the past 150 years, the other concluded it had happened rapidly since the 1950s.

“We detected a specific pattern of ocean cooling south of Greenland and unusual warming off the US coast – which is highly characteristic for a slowdown of the Atlantic overturning, also called the Gulf Stream system,” said Levke Caesar from the Potsdam Institute for Climate Impact Research, the lead author of one of the studies.

“It is practically like a fingerprint of a weakening of these ocean currents.”

The circulation of the Atlantic Ocean plays a key role in regulating global climate. The constantly moving system of deep-water circulation, sometimes referred to as the Global Ocean Conveyor Belt, sends warm, salty Gulf Stream water to the North Atlantic where it releases heat to the atmosphere and warms Western Europe. The cooler water then sinks to great depths and travels all the way to Antarctica and eventually circulates back up to the Gulf Stream (Intergovernmental Panel on Climate Change)

While computer simulations have long predicted changes in ocean circulation, brought about by rising carbon dioxide levels, these studies provide direct proof this is happening.

“The evidence we’re now able to provide is the most robust to date,” said Professor Stefan Rahmstorf from the Potsdam Institute, who conceived the study with Ms Caesar.

“We’ve analysed all the available sea surface temperature datasets, comprising data from the late 19th century until the present.”

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The other study used ocean sediments to explore the weakening Amoc over a longer period of time.

Taken together, the studies provide a comprehensive analysis of the phenomenon, and the scientists suggest climate change is likely to be driving the effects they are seeing.

Increased rainfall as well as melt water from Arctic sea ice – both of which are the result of global warming – are thought to be diluting the waters of the northern Atlantic.

This reduces the ocean’s salt content, making it less dense and stopping water from sinking to the seabed. This in turn slows down Amoc, which is driven by the flux of water with different densities.

Previous work has demonstrated that the decline of Amoc has the potential to exacerbate sea level rise in coastal US cities like New York and Boston, as well driving extreme weather events such as storms and even heatwaves.

While the recent studies did not attempt to predict the future of Amoc, the researchers warned that climate change is likely to continue driving this worrying trend.

“If we do not rapidly stop global warming, we must expect a further long-term slowdown of the Atlantic overturning,” said Dr Alexander Robinson of the University of Madrid, one of the study authors.