Nothing
new here except that a small amount of sanitised truth may be seeping
into the proceedings.
Interesting
idea that the earth itself might undermine a Paris climate agreement.
How
inconvenient!
Tim
Groser and Paula Bennett (once she's learnt what the climate
is) will be seething.
Enough
to turn someone to drink.
Scientists
just pointed out how the Earth itself could undermine a Paris climate
agreement
9
December, 2015
PARIS
— With only three days left, tensions
here are rising as
countries race to resolve outstanding differences and forge an
agreement that — hopefully — will set the planet on a path to
avoiding the worst consequences of climate change.
The
goal is an agreement that would set the world on a path to limit
warming to below 2 degrees Celsius, or perhaps even 1.5
degrees Celsius,
above pre-industrial levels. But at a news conference here at
the Le Bourget conference center Wednesday morning, scientists
pointed out a factor that could make hitting these targets quite
a lot harder.
As
the planet warms, this frozen northern soil is going to continue to
thaw — and as it thaws, it’s going to release carbon dioxide and
methane into the air. A lot of it, it turns out. Potentially enough
to really throw off the carbon
budgets that
have been calculated in order to determine the maximum emissions that
we can release and still have a good chance of keeping warming to 2 C
or below it.
In
particular, Susan Natali of the Woods Hole Research Center explained
Wednesday that with a very high level of warming, permafrost
emissions this century could be quite large indeed.
Natali
used numbers from the 2013
report of
the United Nations’ Intergovernmental Panel on Climate Change,
which found that humans can only emit about 275 more gigatons, or
billion tons, of carbon (about 1,000 gigatons of carbon dioxide,
which has a greater molecular weight) to have a greater than 66
percent chance of limiting warming to 2 degrees C.
But
out of that limited budget, she said, permafrost emissions could take
up some 150 of those gigatons (or about 550 gigatons of carbon
dioxide).
“That’s
on par with current U.S. rates of emission,” Natali said, which are
about 1.4 gigatons of carbon per year. “So we’re talking about
another emitting region that’s currently not included in our
emissions scenarios.”
Fortunately,
even though they’re not considered to be strong enough, the current
national pledges to limit global warming appear to have taken the
world off a truly high emissions path. These pledges, or “intended
nationally determined contributions,” could potentially limit
warming to 2.7 degrees Celsius, according
to the
United Nations.
But
in an interview, Natali and her Woods Hole colleague and fellow
permafrost expert Max Holmes explained that even for lower warming
scenarios like this, permafrost could emit 50 gigatons of carbon (or
about 180 gigatons of carbon dioxide) in this century. This is
because under lower warming scenarios, only about 30 percent, rather
than about 70 percent, of surface layer permafrost is expected to
thaw.
In this Aug. 10, 2009 photo, a hill of permafrost “slumping” from global warming near the remote, boggy fringe of North America, 2,200 kilometers (1,400 miles) from the North Pole.(AP Photo/Rick Bowmer)
Another
50 gigatons out of a 275 gigaton carbon budget — or, another 180
gigatons out of a 1,000 gigaton carbon dioxide budget — would
significantly constrain how much the world could emit and still have
a strong chance of keeping warming below 2 degrees Celsius.
Another
prominent research institute, the U.K. Met Office’s Hadley Center,
also recently
released an
assessment of how potential permafrost emissions could complicate
attempts to limit global warming, and came up with numbers that are,
if anything, potentially even worse. As the center put it:
The
feedbacks from wetlands and permafrost regions can be combined with
other known processes to determine their greenhouse gas input into
the atmosphere. For a global average temperature rise of 2 °C, this
reduces the cumulative emissions that can be released by human
actions by around 100GtC (360 GtCO2 ) in the most pessimistic
simulation. This corresponds to about 10 years of anthropogenic
emissions at the current rate.
These
numbers can’t be directly compared with the Woods Hole numbers,
however, due to the inclusion of wetlands above.
And
Natali and Holmes also noted that permafrost emissions don’t end at
2100 — they are expected to continue after that and even get worse.
“Most of the release will happen after 2100,” said Natali.
That’s
a big problem because the global carbon budget is fixed, and after it
is exceeded there can be zero further emissions. Because carbon
dioxide lasts so long in the atmosphere, you don’t get to start
with a fresh budget in the next century. So permafrost emissions
beyond 2100 would also have to be taken into account, and would
restrict the budget even further.
Permafrost
is a potential carbon bomb because over thousands of years, dead
plant life has been slowly swallowed up by the soil but has not
decomposed. Plants pull carbon out of the atmosphere as they grow,
but release it again when they die and decompose. As permafrost warms
and thaws, microbes will have more ability to break down the plant
life it contains, which is what will trigger a steady stream of
emissions.
“It’s
just like you put celery in your freezer and then you turn your
freezer into a refrigerator, and it starts to rot,” says Woods
Hole’s Max Holmes.
Many
people are confused about permafrost, and think when they first hear
about it that it is going to release methane, not carbon dioxide, in
gigantic explosions. Actually, that’s confusing frozen
subsea methane hydrates —
which may or may not be destabilized by global warming, but in any
case are a separate issue — with permafrost on land.
The
latter will lose carbon slowly, as thaw enables microbial processes
that lead to decomposition. This will release both carbon dioxide and
also some methane. There won’t be any explosion, says Natali —
but as the numbers above show, it could still be dramatically
significant to the total global carbon picture.
The
news about permafrost has been building in recent years, but it is
still a relatively new area of scientific inquiry and one where there
is much uncertainty. Thus, even as negotiators in Paris appear to be
amping up their ambition and are even talking more about trying to
limit global warming to 1.5 degrees C, there may be another wild card
they have to contend with.
On
Tuesday, Secretary of State John F. Kerry called the
Paris climate meeting the “demarcation point where we begin to get
the job done to save the planet.” Alas, scientists are learning
that the planet itself may not cooperate.
Climate
outlook may be worse than feared, global study suggests
9
December, 2015
As
world leaders hold climate talks in Paris, research shows that land
surface temperatures may rise by an average of almost 8C by 2100, if
significant efforts are not made to counteract climate change.
Such
a rise would have a devastating impact on life on Earth. It would
place billions of people at risk fromextreme
temperatures,
flooding, regional drought, and food
shortages.
The
study calculated the likely effect of increasing atmospheric levels
of greenhouse gases above pre-industrialisation amounts. It finds
that if emissions continue to grow at current rates, with no
significant action taken by society, then by 2100 global land
temperatures will have increased by 7.9C, compared with 1750.
This
finding lies at the very uppermost range of temperature rise as
calculated by the Intergovernmental Panel on Climate Change. It also
breaches the United Nations' safe limit of 2C, beyond which the UN
says dangerous climate change can be expected.
Research
at the University of Edinburgh first created a simple algorithm to
determine the key factors shaping climate change and then estimated
their likely impact on the world's land and ocean
temperatures.
The method is more direct and straightforward than that used by the
IPCC, which uses sophisticated, but more opaque, computer models.
The
study was based on historical temperatures and emissions data. It
accounted for atmospheric pollution effects that have been cooling
Earth by reflecting sunlight into space, and for the slow response
time of the ocean.
Its
findings, published in Earth
and Environmental Transactions of the Royal Society of Edinburgh,
may also help resolve debate over temporary slow-downs in temperature
rise.
Professor
Roy Thompson, of the University of Edinburgh's School of GeoSciences,
who carried out the study, said: "Estimates vary over the
impacts of climate
change.
But what is now clear is that society needs to take firm, speedy
action to minimise climate damage."
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