But an avalanche of cold water from the melting Greenland ice sheet appears to be slowing the ocean circulation to levels not experienced in more than 1,000 years.
That’s the conclusion of a bold new attempt to combine temperature measurements and climate-related data scrounged from coral samples, ice cores and tree rings to track the worrying decline of the critical Atlantic Ocean phenomenon. The new research, published Monday in Nature Climate Change, used observations and studies of sea-surface temperatures to produce a new index — one that charts the waning force of the Atlantic meridional overturning circulation (AMOC), one of the planet’s most important circulation systems.
The index reveals a modern powering down of the AMOC, including a sharp slowdown between 1970 and 1990, which had already been widely detected, followed by a partial recovery that nonetheless failed to boost the system back to its vigorous pre-Industrial Revolution state.
If the climate relationships identified by the researchers, led by the Potsdam Institute for Climate Impact Research in Germany, hold true, growing melt rates in Greenland “might lead to further weakening of the AMOC within a decade or two, and possibly even more permanent shutdown” of key components of it, the scientists warn in their paper.
The findings of the research were “dramatic,” but consistent with projections from computer climate models, Stephen Griffies, a National Oceanic and Atmospheric Administration climate and ocean modeler, said. Griffies wasn’t involved with the study. He contributed to recent research linking abrupt AMOC changes with a historically unprecedented five-inch spike in sea levels along Northeast U.S. coastlines in 2009 and 2010. Other researchers have linked that same AMOC slowdown of five years ago with harsh winters in Europe and with a spike in hurricane activity.
“It’s inevitable, from my perspective, that we will start to see more and more evidence for the slowdown of the circulation,” Griffies said. “If the overturning circulation slows down further, these extreme sea-level events on the East Coast will become more frequent.”
Michael Mann, a Penn State professor who directs the school’s Earth System Science Center, and one of the authors of the new study, said Greenland’s ice is melting faster than anticipated, which could explain why the AMOC appears to be slowing “decades ahead of schedule.” He said the abrupt slowdown in the AMOC around 1970 “looked like an aborted collapse” — and that a “full-on collapse” could be possible in the decades ahead.
The precise consequences of an ongoing AMOC slowdown are hard to predict, according to Mann, but he warned that it could reduce global food security by withholding deepsea nutrients from fisheries and food chains that flourish in shallower Atlantic Ocean depths.
“The most productive region, in terms of availability of nutrients, is the high latitudes of the North Atlantic,” Mann said. “If we lose that, that’s a fundamental threat to our ability to continue to fish.”
Without the AMOC to carry heat away from the tropics and redistribute it, Mann said parts of the Northern Hemisphere could become cooler. But he also said hurricanes, Nor’easters and other storms could become more common, providing the heat with an alternative pathway along which it can travel.
“If you shut down this mode of ocean circulation, you’re denying the climate system one of its modes of heat transport,” Mann said. “if you deny it one mode of transport, it’s often the case that you will see other modes of transport increase.”
Read more at Atlantic Circulation Weaker Than in Last Thousand Years
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