Billions of tonnes of meltwater flowing into the world’s oceans from the Greenland and Antarctic ice sheets could boost extreme weather and destabilise regional climate in a matter of decades, researchers said.
The melting ice giants, especially the one atop Greenland, are poised to further weaken the ocean currents that move cold water south along the Atlantic Ocean’s floor, while pushing tropical waters northward closer to the surface, scientists reported in the journal, Nature.
Known as the Atlantic Meridional Overturning Circulation (AMOC), this liquid conveyor belt plays a crucial role in Earth’s climate system and helps ensure the relative warmth of the Northern Hemisphere.
“According to our models, this meltwater will cause significant disruptions to ocean currents and change levels of warming around the world,” said lead author Nicholas Golledge, an associate professor at the Antarctic Research Centre of New Zealand’s Victoria University of Wellington.
The Antarctic ice sheet’s loss of mass, meanwhile, traps warmer water below the surface, eroding glaciers from underneath in a vicious circle of accelerated melting that contributes to sea level rise.
Most studies on ice sheets have focused on how quickly they might shrink from climate change and how much global temperatures can rise before their disintegration becomes inevitable, a threshold known as a “tipping point”.
But far less research has been done on how the meltwater might affect the climate system itself.
More extreme weather
“The large-scale changes we see in our simulations are conducive to a more chaotic climate with more extreme weather events and more intense and frequent heat waves,” said co-author Natalya Gomez, a researcher in the Department of Earth and Planetary Sciences at McGill University in Canada.
Researchers concluded that, by mid-century, meltwater from the Greenland ice sheet will noticeably disrupt AMOC, which has already shown signs of slowing down.
This is a “much shorter timescale than expected”, noted Helene Seroussi, a researcher in the Sea Level and Ice Group at the Jet Propulsion Laboratory in California, who was not involved in the study.
The findings were based on highly detailed simulations combined with satellite observations of changes to the ice sheets since 2010.
The Antarctic and Greenland ice sheets, up to 3km thick, contain more than two-thirds of the planet’s fresh water, enough to raise global oceans 58 and 7 metres, respectively, were they to melt completely.
Off the ice cliff
Besides Greenland, the regions most vulnerable to global warming are West Antarctica and several huge glaciers in East Antarctica, which is far larger and more stable.
In a second study published Wednesday in Nature, some of the same scientists offered new projections of how much Antarctica will contribute to sea level rise by 2100 – a hotly debated topic.
A controversial 2016 study suggested the continent’s ice cliffs – exposed by the disintegration of ice shelves that jut out from glaciers over ocean water – were highly vulnerable to collapse, and could lead to sea level rise of a metre by century’s end.
That would be enough to displace up to 187 million people around the world, especially in populous, low-lying river deltas in Asia and Africa, research has shown.
But the new study challenges those findings.
“Unstable ice-cliffs were proposed as a cause of unstoppable collapse of large parts of the ice sheet,” said lead author Tamsin Edwards, a lecturer in geography at King’s College London.
“But we’ve re-analysed the data and found this isn’t the case.”
Both of the new studies, Edwards said “predict a most likely Antarctic contribution of 15 centimetres” by 2100, with an upward limit of about 40cm.
A special report on oceans by the UN’s Intergovernmental Panel on Climate Change (IPCC), due out in September, will offer a much-anticipated estimate of sea level rise.
The IPCC’s last major assessment in 2013 did not take ice sheets, today seen as the major contributor, ahead of thermal expansion and glaciers, into account because of a lack of data.