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Tuesday, 7 August 2018
Domino-effect of climate events could push Earth into a ‘hothouse’ state
Polar bears on sea ice: the loss of the Greenland ice sheet could
disrupt the Gulf Stream, which would in turn raise sea levels and
accelerate Antarctic ice loss.
Photograph: Paul Goldstein/Cover Images
A domino-like cascade of melting ice, warming seas, shifting currents
and dying forests could tilt the Earth into a “hothouse” state beyond
which human efforts to reduce emissions will be increasingly futile, a
group of leading climate scientists has warned.
This grim prospect is sketched out in a journal paper that considers
the combined consequences of 10 climate change processes, including the
release of methane trapped in Siberian permafrost and the impact of
melting ice in Greenland on the Antarctic.
The authors of the essay, published in Proceedings of the National Academy of Sciences,
stress their analysis is not conclusive, but warn the Paris commitment
to keep warming at 2C above pre-industrial levels may not be enough to
“park” the planet’s climate at a stable temperature.
They warn that the hothouse trajectory “would almost certainly flood
deltaic environments, increase the risk of damage from coastal storms,
and eliminate coral reefs (and all of the benefits that they provide for
societies) by the end of this century or earlier.”
"Fifty years ago, this would be dismissed as alarmist, but now scientists have become really worried"
“I
do hope we are wrong, but as scientists we have a responsibility to
explore whether this is real,” said Johan Rockström, executive director
of the Stockholm Resilience Centre. “We need to know now. It’s so
urgent. This is one of the most existential questions in science.”
Rockström and his co-authors are among the world’s leading
authorities on positive feedback loops, by which warming temperatures
release new sources of greenhouse gases or destroy the Earth’s ability
to absorb carbon or reflect heat.
Their new paper asks whether the planet’s temperature can stabilise
at 2C or whether it will gravitate towards a more extreme state. The
authors attempt to assess whether warming can be halted or whether it
will tip towards a “hothouse” world that is 4C warmer than
pre-industrial times and far less supportive of human life.
Katherine Richardson from the University of Copenhagen, one of the
authors, said the paper showed that climate action was not just a case
of turning the knob on emissions, but of understanding how various
factors interact at a global level.
“We note that the Earth has never in its history had a quasi-stable
state that is around 2C warmer than the preindustrial and suggest that
there is substantial risk that the system, itself, will ‘want’ to
continue warming because of all of these other processes – even if we
stop emissions,” she said. “This implies not only reducing emissions but
much more.”
New feedback loops are still being discovered. A separate paper published in PNAS reveals
that increased rainfall – a symptom of climate change in some regions -
is making it harder for forest soils to trap greenhouse gases such as
methane.
Previous studies have shown that weakening carbon sinks will add
0.25C, forest dieback will add 0.11C, permafrost thaw will add 0.9C and
increased bacterial respiration will add 0.02C. The authors of the new
paper also look at the loss of methane hydrates from the ocean floor and
the reduction of snow and ice cover at the poles.
Rockström says there are huge gaps in data and knowledge about how
one process might amplify another. Contrary to the Gaia theory, which
suggests the Earth has a self-righting tendency, he says the feedbacks
could push the planet to a more extreme state.
As
an example, the authors say the loss of Greenland ice could disrupt the
Gulf Stream ocean current, which would raise sea levels and accumulate
heat in the Southern Ocean, which would in turn accelerate ice loss from
the east Antarctic. Concerns about this possibility were heightened
earlier this year by reports that the Gulf Stream was at its weakest level in 1,600 years.
Currently, global average temperatures are just over 1C above
pre-industrial levels and rising at 0.17C per decade. The Paris climate
agreement set actions to keep warming limited to 1.5C-2C by the end of
the century, but the authors warn more drastic action may be necessary.
“The heatwave we now have in Europe is not something that was
expected with just 1C of warming,” Rockström said. “Several positive
feedback loops are already in operation, but they are still weak. We
need studies to show when they might cause a runaway effect.
Another climate scientist – who was not involved in the paper –
emphasised the document aimed to raise questions rather than prove a
theory. “It’s rather selective, but not outlandish,” said Prof Martin
Siegert, co-director of the Grantham Institute.
“Threshold and tipping points have been discussed previously, but to
state that 2C is a threshold we can’t pull back from is new, I think.
I’m not sure what ‘evidence’ there is for this – or indeed whether there
can be until we experience it.”
Rockström said the question needed asking. “We could end up
delivering the Paris agreement and keep to 2C of warming, but then face
an ugly surprise if the system starts to slip away,” he said. “We don’t
say this will definitely happen. We just list all the disruptive events
and come up with plausible occurrences … 50 years ago, this would be
dismissed as alarmist, but now scientists have become really worried.”
“In the context of the summer of 2018, this is definitely not a case
of crying wolf, raising a false alarm: the wolves are now in sight,”
said Dr Phil Williamson, a climate researcher at the University of East
Anglia. “The authors argue that we need to be much more proactive in
that regard, not just ending greenhouse gas emissions as rapidly as
possible, but also building resilience in the context of complex Earth
system processes that we might not fully understand until it is too
late.”
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