Scientists predict a collapse of the Atlantic ocean current to happen mid-century
University of Copenhagen - Faculty of Science
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| From the "Day After Tomorrow (2004) after the Gulf Stream collapses and the ocean inundates the land. No Jake Gyllenhaal to rescue us |
This is the conclusion based on new calculations that contradict the
latest report from the IPCC.
Important ocean currents that redistribute heat, cold and precipitation between the tropics and the northernmost parts of the Atlantic region will shut down around the year 2060 if current greenhouse gas emissions persist. This is the conclusion based on new calculations from the University of Copenhagen that contradict the latest report from the IPCC.
Contrary to what we may imagine about the impact of climate
change in Europe, a colder future may be in store. In a new study, researchers
from the University of Copenhagen's Niels Bohr Institute and Department of
Mathematical Sciences predict that the system of ocean currents which currently
distributes cold and heat between the North Atlantic region and tropics will
completely stop if we continue to emit the same levels of greenhouse gases as
we do today.
Using advanced statistical tools and ocean temperature data
from the last 150 years, the researchers calculated that the ocean current,
known as the Thermohaline Circulation or the Atlantic Meridional Overturning
Circulation (AMOC), will collapse -- with 95 percent certainty -- between 2025
and 2095. This will most likely occur in 34 years, in 2057, and could result in
major challenges, particularly warming in the tropics and increased storminess
in the North Atlantic region.
"Shutting down the AMOC can have very serious consequences for Earth's climate, for example, by changing how heat and precipitation are distributed globally. While a cooling of Europe may seem less severe as the globe as a whole becomes warmer and heat waves occur more frequently, this shutdown will contribute to an increased warming of the tropics, where rising temperatures have already given rise to challenging living conditions," says Professor Peter Ditlevsen from the Niels Bohr Institute.
"Our result underscores the importance of reducing
global greenhouse gas emissions as soon as possible," says the researcher.
The calculations, just published in the scientific
journal, Nature Communications, contradict the message of the
latest IPCC report, which, based on climate model simulations, considers an
abrupt change in the thermohaline circulation very unlikely during this
century.
Early warning signals present
The researchers' prediction is based on observations of
early warning signals that ocean currents exhibit as they become unstable.
These Early Warning Signals for the Thermohaline Circulation
have been reported previously, but only now has the development of advanced
statistical methods made it possible to predict just when a collapse will
occur.
The researchers analysed sea surface temperatures in a
specific area of the North Atlantic from 1870 to present days. These sea
surface temperatures are "fingerprints" testifying the strength of
the AMOC, which has only been measured directly for the past 15 years.
"Using new and improved statistical tools, we've made
calculations that provide a more robust estimate of when a collapse of the
Thermohaline Circulation is most likely to occur, something we had not been
able to do before," explains Professor Susanne Ditlevsen of UCPH's
Department of Mathematical Sciences.
The thermohaline circulation has operated in its present mode since the last ice age, where the circulation was indeed collapsed. Abrupt climate jumps between the present state of the AMOC and the collapsed state has been observed to happen 25 times in connection with ice age climate.
These are
the famed Dansgaard-Oeschger events first observed in ice cores from the
Greenlandic ice sheet. At those events climate changes were extreme with 10-15
degrees changes over a decade, while present days climate change is 1.5 degrees
warming over a century.
Facts:
·
The Atlantic Meridional Overturning Circulation (AMOC) is
part of a global system of ocean currents. By far, it accounts for the most
significant part of heat redistribution from the tropics to the northernmost
regions of the Atlantic region -- not least to Western Europe.
·
At the northernmost latitudes, circulation ensures that
surface water is converted into deep, southbound ocean currents. The
transformation creates space for additional surface water to be moved northward
from equatorial regions. As such, thermohaline circulation is critical for
maintaining the relatively mild climate of the North Atlantic region.
· The work is supported by TiPES, a joint-European research collaboration focused on tipping points of the climate system. The TiPES project is an EU Horizon 2020 interdisciplinary climate research project focused on tipping points in the climate system.
