While the melting of the Greenland ice sheet is expected to slow or even collapse the Atlantic Ocean current that keeps Europe warm, meltwater from West Antarctica could preserve this vital current.
But it won’t be enough to prevent major changes in the climate. The Atlantic Meridional Overturning Circulation (AMOC) would still decline by 60 per cent, and its full recovery would take 3000 years.
“I would tend to say, don’t be so quick to say that the AMOC is going to collapse,” says Sacha Sinet at Utrecht University in the Netherlands. “But the things I show here do not change much what will happen for the next century. Probably you will not be alive to tell if the AMOC was stabilised or not by West Antarctica.”
The AMOC is a system of currents that brings warm surface water from the tropics towards northern Europe, where it cools and sinks before flowing south to Antarctica. The current carries 1.2 petawatts of heat – equivalent to the energy generated by 1 million power plants – that keeps Europe much warmer than Labrador or Siberia at the same latitude. But light, fresh meltwater from Greenland’s ice is expected to hinder the sinking of salty, dense AMOC water, slowing down the current.
If the AMOC collapsed, winter cold snaps could reach almost -50°C (-58°F) in northern Europe. This week, Iceland declared AMOC shutdown an “existential” security threat. Sea levels would also be higher along the US east coast, and Africa could suffer more severe droughts.
Continue reading “Research: Antarctic Melt Could Save AMOC, But Wait…”




