Critical ocean system may be heading for collapse due to climate change study finds
Human-caused warming has led to an âalmost complete loss of stabilityâ in the system that drives Atlantic Ocean currents, a new study has found â" raising the worrying prospect that this critical aquatic âconveyer beltâ could be close to collapse.
In recent years, scientists have warned about a weakening of the Atlantic Meridional Overturning Circulation (AMOC), which transports warm, salty water from the tropics to northern Europe and then sends colder water back south along the ocean floor. Researchers who study ancient climate change have also uncovered evidence that the AMOC can turn off abruptly, causing wild temperature swings and other dramatic shifts in global weather systems.
An influx of freshwater from melting ice sheets and glaciers is diluting the North Atlanticâs saltiness.Credit:AP
Scientists havenât directly observed the AMOC slowing down. But the new analysis, published on Thursday in the journal Nature Climate Change, draws on more than a century of ocean temperature and salinity data to show significant changes in eight indirect measures of the circulationâs strength.
These indicators suggest that the AMOC is running out of steam, making it more susceptible to disruptions that might knock it out of equilibrium, says study author Niklas Boers, a researcher at the Potsdam Institute for Climate Impact Science in Germany.
If the circulation shuts down, it could bring extreme cold to Europe and parts of North America, raise sea levels along the east coast of the United States and disrupt seasonal monsoons that provide water to much of the world.
âThis is an increase in understanding ... of how close to a tipping point the AMOC might already be,â said Levke Caesar, a climate physicist at Maynooth University who was not involved in the study.
Boersâ analysis doesnât suggest exactly when the switch might happen. But âthe mere possibility that the AMOC tipping point is close should be motivation enough for us to take countermeasures,â Caesar said. âThe consequences of a collapse would likely be far-reaching.â
The AMOC is the product of a gigantic, ocean-wide balancing act. It starts in the tropics, where high temperatures not only warm up the seawater but increase its proportion of salt by boosting evaporation. This warm, salty water flows north-east from the US coastline toward Europe â" creating the current we know as the Gulf Stream.
But as the current gains latitude it cools, adding density to waters already laden with salt. By the time it hits Greenland it is dense enough to sink deep beneath the surface. It pushes other submerged water south toward Antarctica, where it mixes with other ocean currents as part of a global system known as the âthermohaline circulationâ.
This circulation is at the heart of Earthâs climate system, playing a critical role in redistributing heat and regulating weather patterns around the world.
As long as the necessary temperature and salinity gradients exist, AMOC is self-sustaining, Boers explained. The predictable physics that makes dense water sink and lighter water âupwellâ keeps the circulation churning in an endless loop.
But climate change has shifted the balance. Higher temperatures make ocean waters warmer and lighter. An influx of freshwater from melting ice sheets and glaciers dilutes North Atlanticâs saltiness, reducing its density. If these waters arenât heavy enough to sink, the entire AMOC will shut down.
Itâs happened before. Studies suggest that, toward the end of the last ice age, a massive glacial lake burst through a declining North American ice sheet. The flood of freshwater spilled into the Atlantic, halting the AMOC and plunging much of the northern hemisphere â" especially Europe â" into deep cold. Gas bubbles trapped in polar ice indicate the cold spell lasted 1000 years. Analyses of plant fossils and ancient artifacts suggest that the climate shift transformed ecosystems and threw human societies into upheaval.
âThe phenomenon is intrinsically bi-stable,â Woods Hole Oceanographic Institution president Peter de Menocal said of the AMOC. âItâs either on or itâs off.â
But is it about to turn off now?
âThatâs the core question weâre all concerned about,â said de Menocal, who was not involved in Boersâs research.
In its 2019 âSpecial Report on the Ocean and Cryosphere in a Changing Climate,â the United Nations Intergovernmental Panel on Climate Change projected that the AMOC would weaken during this century, but total collapse within the next 300 years was only likely under the worst-case warming scenarios.
The new analysis suggests âthe critical threshold is most likely much closer than we would have expected,â Boers said.
The ârestoring forces,â or feedback loops, that keep the AMOC churning are in decline, he said. All the indicators analysed in his study â" including sea surface temperature and salt concentrations â" have become increasingly variable.
Itâs as though the AMOC is a patient newly arrived in the emergency room, and Boers has provided scientists with an assessment of its vital signs, de Menocal said. âAll the signs are consistent with the patient having a real mortal problem.â
Physical oceanographers like him are also trying to confirm the AMOC slowdown through direct observations. But the AMOC is so big and complex it will likely take years of careful monitoring and data collection before a definitive measurement is possible
âYet everyone also realises the jeopardy of waiting for that proof,â de Menocal said.
After all, there are plenty of other indications that Earthâs climate is in unprecedented territory. This northern hemisphere summer, the Pacific Northwest was blasted by a heat wave scientists say was âvirtually impossibleâ without human-caused warming. China, Central Europe, Uganda and India have all experienced massive, deadly floods. Wildfires are ranging from California to Turkey to the frozen forests of Siberia.
The world is more than 1 degree warmer than it was before humans started burning fossil fuels, and itâs getting hotter all the time.
And the apparent consequences of the AMOC slowing are already being felt. A persistent âcold blobâ in the ocean south of Greenland is thought to result from less warm water reaching that region. The lagging Gulf Stream has caused exceptionally high sea level rise along the east coast of the United States. Key fisheries have been upended by the rapid temperature swings, and beloved species are struggling to cope with the changes.
If the AMOC does completely shut down, the change would be irreversible in human lifetimes, Boers said. The âbi-stableâ nature of the phenomenon means it will find new equilibrium in its âoffâ state. Turning it back on would require a shift in the climate far greater than the changes that triggered the shutdown.
âItâs one of those events that should not happen, and we should try all that we can to reduce greenhouse gas emissions as quickly as possible,â Boers said. âThis is a system we donât want to mess with.â
The Washington Post
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