How Earth's oceans plunged the planet into a catastrophic big freeze - and it wasn't caused by humans
Nov 7, 2012 | Damien Gayle
The planet's last major cold spell 13,000 years ago was caused by a
catastrophic deluge of frigid fresh water from north-west Canada into
the Arctic ocean, a new study suggests. Detailed computer simulations
show meltwater from the enormous Laurentide Ice Sheet halted the sinking
of very dense, saltier, colder water in the North Atlantic.
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Detailed: A new model of flood waters from the
melting Laurentide Ice Sheet shows how water first flowed north-west
into the Arctic, weakening deep ocean circulation and leading to the
Earth's last major cold period |
That stopped the large scale ocean circulation - the so-called
thermohaline circulation - that transports heat to Europe and North
America, causing the continents to dramatically freeze. The findings
offer a new explanation for the cause of this last big chill, which
scientists had thought was caused by freshwater flowing into the
Atlantic through Canada's Gulf of St Lawrence.
It led to a cold spell lasting more than 1,000 years known as the
Younger Dryas or 'Big Freeze', during which temperatures in parts of the
northern hemisphere fell to about 10 degrees C colder than they are
today.
'This episode was the last time the Earth underwent a
major cooling, so understanding exactly what caused it is very
important for understanding how our modern-day climate might change in
the future,' said Alan Condron, of the University of Massachusetts
Amherst.
The cooling began after Lake Agassiz, at the southern edge of the
Laurentide ice sheet covering much of the Canadian Arctic, broke through
an ice dam and dumped thousands of cubic kilometers of cold water into
the ocean.
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© AP
Argentina's
Patagonia ice-sheet: Much of Europe and North America would have looked
like this after the meltwater from the Laurentide Ice Sheet brought
about a dramatic global cooling |
Using a high resolution, global, ocean-ice circulation model 10 to 20
times more powerful than previous ones, the researchers compared how
meltwater from the two different drainage outlets affected ocean
circulation.
The original hypothesis, proposed 1989 by Wally Broecker of Columbia
University, suggested that Lake Aggasiz drained into the North Atlantic
down the St Lawrence River.
But using the new model, Dr Condron, working with Peter Winsor of the
University of Alaska, found that this proposed route would have weakened
the oceans' thermohaline circulation by less than 15 per cent.
That level of weakening, they say, is unlikely to have accounted for the 1,000-year cold climate event that followed the flood.
Meltwater from the St Lawrence River actually ends up almost 1,900 miles
south of the deep water formation regions, too far south to have any
significant impact on the sinking of surface waters.
By contrast, Dr Condron and Dr Winsor's model shows that if the
meltwater first drains into the Arctic Ocean, narrow coastal boundary
currents efficiently deliver it to the deep water formation regions of
the sub-polar north Atlantic, weakening the thermohaline circulation by
more than 30 per cent.
They conclude that this scenario, showing meltwater discharged first
into the Arctic rather than down the St. Lawrence valley, is 'more
likely to have triggered the Younger Dryas cooling.'
Dr Condron and Dr Winsor ran their simulations on one of the world's top
supercomputers at the National Energy Research Science Computing Centre
in Berkeley, California.
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Reporting their findings in the journal Proceedings of the National
Academy of Sciences, they wrote: 'With this higher resolution modelling,
our ability to capture narrow ocean currents dramatically improves our
understanding of where the fresh water may be going.'
Dr Condron added: 'The results we obtain are only possible by using a
much higher computational power available with faster computers.
'Older models weren't powerful enough to model the different pathways
because they contained too few data points to capture smaller-scale,
faster-moving coastal currents.'
'Our results are particularly relevant for how we model the melting of
the Greenland and Antarctic Ice sheets now and in the future.
'It is apparent from our results that climate scientists are
artificially introducing fresh water into their models over large parts
of the ocean that freshwater would never have reached.
'In addition, our work points to the Arctic as a primary trigger for
climate change. This is especially relevant considering the rapid
changes that have been occurring in this region in the last 10 years.'