The Atlantic Ocean’s current system, an engine of the Northern Hemisphere’s climate, could be weakening due to climate change, which could have severe consequences for the world’s weather including “extreme cold” in Europe and parts of North America and rising sea levels in parts of the United States, according to a new scientific study.
The Atlantic Meridional Overturning Circulation (AMOC) is part of a large system of ocean currents, known as the Gulf Stream, that transports warm water from the tropics northwards into the North Atlantic.
“The loss of dynamical stability would imply that the AMOC has approached its critical threshold, beyond which a substantial and in practice likely irreversible transition to the weak mode could occur,” said Niklas Boers at the Potsdam Institute for Climate Impact Research and author of the study published on Thursday.
As the atmosphere warms due to increased greenhouse gas emissions, the surface ocean beneath retains more heat. A potential collapse of the system could have severe consequences for the world’s weather systems, according to the study.
If the AMOC collapsed, it would increase cooling in the Northern Hemisphere, contribute to rising sea levels in the Atlantic, an overall fall in precipitation over Europe and North America and a shift in monsoons in South America and Africa, Britain’s Meteorological or Met Office warned.
Read also: COVID-19 in Africa peaks with 6,400 deaths recorded, says WHO
In April, the United Nations had warned that the world is on the verge of climate crisis “abyss”, as Secretary-General Antonio Guterres urged countries to “end our war on nature”.
Related Posts
Climate change has been blamed for the extreme weather conditions that has hit parts of the world in recent weeks and months – from the deadly wildfires in Turkey and Greece to the flooding in many parts of Asia including China, where more than 300 died.
Climate models have already shown that the AMOC is at its weakest in more than a 1,000 years.
However, it has not been known whether the weakening is due to a change in circulation or a loss of stability.
The study, published in the journal Nature Climate Change, said the difference is crucial.
“The findings support the assessment that the AMOC decline is not just a fluctuation or a linear response to increasing temperatures but likely means the approaching of a critical threshold beyond which the circulation system could collapse,” Boers said.
Other climate models have said the AMOC will weaken over the coming century but that a collapse before 2100 is unlikely.
Source: Aljazeera
