http://www.350resources.org.uk/2013/02/28/arctic-melt-may-be-the-first-tipping-point-that-triggers-many-more/

Arctic melt may be the first tipping point that triggers many more

28/2/2013 New Scientist

Arctic thaw may be first in cascade of tipping points.   – by Michael
Marshall.

One climate domino has fallen, and it may start toppling others. A recent
study outlined an interconnected web of climate tipping points, some of
which make the next ones more likely. Now, an analysis of data from the
last 23 years suggests we passed the first of these tipping points in 2007,
when Arctic sea ice flipped into a new, less stable state. That may speed
the world towards the next tipping point – the thaw of a vast expanse of
Siberian permafrost. When it comes to the consequences of climate change,
few are more dramatic than tipping points – a small push unleashes a big
change, which may be unstoppable. According to Tim Lenton of the University
of Exeter, UK, and Valerie Livina of the UK’s National Physical Laboratory,
Earth saw its first tipping point in 2007 when the Arctic sea ice hit a
record low. The pair analysed data on ice cover going back to 1979, and
found that every year since then, the extent of sea ice in the summer has
been hovering around a new, shrunken state (The Cryosphere, doi.org/kkq).
“This wasn’t a one-off, it was a permanent change,” Lenton says. He notes
that since 2007, the ice has consistently taken longer to recover from
small changes, suggesting it has entered a new, less stable state.The claim
is controversial. Anders Levermann of the Potsdam Institute for Climate
Impact Research in Germany argues that the ice loss cannot be called a
tipping point because it could still be reversed. Peter Ditlevsen of the
University of Copenhagen in Denmark says it is clear from the ice cover
data that 2007 marked a dramatic turning point for Arctic sea ice.A little
further south, in the expanse of Siberian permafrost known as Yedoma,
another tipping point could be looming. Ecologists predict that once the
region begins to thaw, microbes will start breaking down the carbon-rich
soil, producing heat and releasing greenhouse gases, which will accelerate
the thaw.Anton Vaks of the University of Oxford and colleagues used
stalagmites in caves beneath Russia and China to reconstruct the
500,000-year history of the Siberian permafrost. Stalagmites cannot form
when the soil is frozen, Vaks explains. “They only grow when water flows
into caves.” He found that those in the northernmost cave – nearest to
modern-day continuous Siberian permafrost – only grew once, during a
particularly warm period 400,000 years ago when global temperatures were
1.5 °C warmer than pre-industrial temperatures. That suggests the
permafrost is likely to become vulnerable when we hit 1.5 °C of global
warming (Science, doi.org/kkt).Global temperatures have already risen by
0.8 °C. Even if humanity stopped all emissions tomorrow, temperatures would
rise another 0.3 °C, suggesting the permafrost tipping point is likely to
be reached.These two tipping points – the Arctic sea ice and permafrost –
are the first two in a network of points outlined recently by Lenton and
Levermann (see diagram). The pair argue that periods of rapid ice loss in
the Arctic change regional weather patterns, to warm Asia more quickly and
speed up the thaw.“No climate model has ever induced the tipping of one by
tipping another,” cautions Levermann. But he says that could be a quirk of
the models, which climate modellers build to study aspects of climate that
don’t involve tipping points. “We observe more violent changes in the past
than our models are capable of simulating,” agrees Ditlevsen. “That points
to the idea of dominoes.”See more: “Tipping point cascade”In Lenton and
Levermann’s cascade, a critical point appears to be the shutdown of the
Atlantic thermohaline circulation. This vast current pumps water around all
the Earth’s oceans, and interacts with many of the other areas susceptible
to tipping points, including the Greenland and Antarctic ice. The good news
is that this tipping point could act as a safety valve, slowing the
progress of the others.There are huge arguments over whether it will ever
be hit. “All the models show the overturning circulation declining with
global warming,” says Levermann. But that doesn’t mean it will collapse.
Ditlevsen and Jan Sedlácek of ETH Zurich in Switzerland believe internal
mechanisms would reboot the circulation in the event of a collapse – in
part because so far, there is no evidence of a complete collapse in the
past.Perhaps the worst news of all is that there may be no warning of
impending flips. Lenton has developed tipping point forecasts that look for
warning signs. Historical records and chaos theory applied to ecosystem
models suggest that as a system nears a threshold, it will struggle to
bounce back from small disturbances. So if a system is approaching a
tipping point, its response to extreme events should become more sluggish.
The trouble is that the one tipping point we have already passed, according
to Lenton – melting of the Arctic sea ice – gave us no such warning signs.
Ditlevsen is not surprised. He found that there was no warning before
similar events during the last ice age either (Geophysical Research
Letters, doi.org/fd7vkj). Both researchers say the behaviour of other
unstable systems, like the Amazon rainforest, glaciers and monsoons, may be
more predictable.So what’s next? According to the temperatures on Lenton
and Levermann’s cascade, the collapse of Greenland’s ice sheet would become
inevitable shortly after the Yedoma permafrost thaws. This would raise sea
levels 7 metres, over many centuries. A 2012 study (Nature Climate Change,
doi.org/kkw) suggested it would only take 1.6 °C, because as soon as the
south-eastern ice sheet starts losing surface mass, the entire sheet
destabilises.

This article appeared in print under the headline
“Domino effect tips climate over edge”

Go to:
http://www.newscientist.com/article/mg21729064.500-arctic-thaw-may-be-first-in-cascade-of-tipping-points.html
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