Recently in Copenhagen Congress Category
Stefan Rahmstorf of Germany's Potsdam Institute stressed
how he sees the 2 degree target for climate change as an absolute upper limit,
not just a guideline. "When politicians talk about an ambition of 2
degrees, if all goes reasonably well we get 3," he said. "As
scientists that really is an upper limit we should not cross. At 2 degrees I
think we have more than a 1 in 6 chance of really bad impacts." This
morning delegates heard John Schellnhuber, director of the Potsdam Institute,
explain how that more than 1 in 6 chance is worse than your odds of survival
when playing Russian Roulette.
Rasmussen, however, was somewhat dismayed by this news.
"I need some concrete advice now," he said. "We had a very hard
battle in the EU to get the 2 degree target, and now you tell me it's not
enough. I need to know and I need to know today."
Will Steffen of Australian National University stepped in
to the debate to explain that coming up with a number is a risk game. He
believes it's up to politicians to decide how much of a risk society is
prepared to take. And while Steffen thinks 2 degrees is a reasonable target for
2009, the situation could change in five years. Rahmstorf insisted he would
advise a more ambitious target if at all possible, one that leaves room for
manoeuvre and a safety margin.
In response, Rasmussen recommended that scientists not
give politicians too many moving targets. "It is already complex," he
said. "I need your help to move this in the right direction." The
process now is for discussion of the agreement at the G8 summit in July, the UN
meeting in September and the December meeting back in Copenhagen. Rasmussen
says there will be three key elements to the agreement - targets, funding and
verification.
With regards to targets, the aim is to cut global
emissions by 50% compared to 1990 levels by 2050. "I have noted that that
should be a minimum," said Rasmussen. A binding agreement should come from
developed countries to cut their emissions substantially by 2020, and by 80% by
2050. Developing countries, meanwhile, should cut their emissions by 15-30% compared
to business-as-usual by 2020, and after that create real reductions.
Developed countries should provide funds to developing
countries to help them transform to a low carbon economy, with forests and land
use as part of the package, continued the prime minister. They should also help
with adaptation and the dissemination of technology. And a reliable and
transparent system is needed to verify international actions, both on emissions
and technology.
"I call on the scientific community to follow the trends
closely and help us adjust our course," said Rasmussen.
Later he laid out the pros and cons of both carbon
trading and carbon tax schemes. "Don't let anyone kid you that a tax
scheme is clearly the best," he said.
Stern put together the Stern Review of the economics of
climate change in 2006 for the UK government. In the light of evidence since
then, he believes his report underestimated the damages climate change could
cause and the speed of that change. Today he says two big challenges face
us - poverty and climate change. And if
we don't fix climate change we will create a physical climate so hostile that
the hard-won gains in development are lost.
"We should be supporting development that is shaped
and driven by developing countries themselves," said Stern. "This is
about working together to expand the options that people have, the technologies
that are available...then there would be a real partnership."
The necessary resources could come from carbon finance,
overseas development assistance, private investment, and the various kinds of
guarantee and insurance instruments available to the international finance
institutions.
Stern stressed that if developed countries can show
examples where they have achieved low-carbon growth, it would be far more
powerful than just talking about it. To date developing countries have only
seen development in the west result from a high-carbon growth path but this
need no longer be the case.
Stern reckons that a high-carbon growth future would kill
itself, firstly from high hydrocarbon costs and then because of climate change.
"We should see action as, rather, attraction and inaction as
inexcusable," he said.
That action is particularly attractive in an economic
slowdown, when resources are cheaper. "Now's the time to get the
unemployed of Europe getting our houses more energy efficient," said
Stern. "We must not sow the seeds of the next bubble. We can come out of
this one and lay the foundations for low carbon growth."
Speaking at a lunchtime workshop at the Climate Change
Congress in Copenhagen, Barker explained how he's keen to bring as many
different modelling approaches to bear on the problem as possible. And he's
looking to bring together representatives from each of the industries to work together
with the relevant scientists, as well as representatives from government and
NGOs.
"The more independent modelling teams the
better," said Barker, who is also looking for short-term funding for the
project. "The results are more convincing if we're coming at them from
different approaches."
If you're interested in participating, send an email to erw36@cam.ac.uk.
But David Hilbert of CSIRO, Australia, has found that the
Australian rainforest has showed a consistent trend of lower tree mass in
warmer climates. Hilbert and colleagues studied 17 sites in north-east Australia
for up to 35 years. There was no trend over time, but both the growth rate and
the mortality rate increased with temperature. (Recruitment rate - the growth
of new trees - was independent of temperature but increased with increasing
mortality). As the mortality rate increased, the basal area - the
cross-sectional area at a height of 1.3 m of all trees larger than 10 cm in diameter,
and an indicator of the amount of carbon stored - decreased.
Hilbert says that the ecosystem feedbacks in global
climate models are based on short term processes such as carbon fixation by
photosynthesis or decomposition, whereas in the longer term stocks of carbon
are controlled by tree demographic processes. "Despite higher tree growth
rates and higher turnover of biomass, rainforests in warmer climates stores
less carbon because of the higher mortality rate," he added.
The team estimates that tropical rainforests will lose 14
Mg of carbon stored per hectare per degree of climate warming. So that means a
total loss of storage in the world's rainforests of 24.5 Pg of carbon per
degree of warming - equivalent to 2.5 times 2007's carbon emissions. If warming
proceeds at 0.05 degrees per year (the maximum IPCC prediction), that would
give a storage loss of 1.2 Pg of carbon per year. Scarily, that's greater than
the amount we assume that the rainforests remove from the atmosphere each year
today.
The complete collapse of the Greenland ice sheet would
lead to around 6.5 m of sea level rise. So scientists are keen to know at what
temperature melting of the ice sheet is likely to become irreversible. A few
years ago Jonathan Gregory calculated this threshold at 3 degrees of
temperature rise but Bamber says there are two lines of evidence that suggest
this is wrong - the past and the modelling future. "I think there are
other processes in there that may be important," he said. In the Eemian
Greenland was about 5 degrees warmer than today, considerably above Gregory's
threshold, but there was still an ice sheet present (although probably about
half its present volume) and it remained in place for 20,000 years.
Bamber has recalculated the critical threshold
temperature for ice sheet melting by forcing two surface mass balance models
with real future climate. The first model, a positive degree day (PDD) model,
which says that the ice sheet will melt if the temperature falls below zero,
gave a temperature threshold of 4 degrees. That figure is comparable to
Gregory's threshold of a 3 degree average global temperature rise, which
corresponds to a temperature increase in Greenland of around 4.5 degrees.
But in Bamber's second calculation the relatively
sophisticated energy balance model, which he believes better represents ice
sheet behaviour, gave a threshold of 8 degrees for irreversible melting of
Greenland - double the previously published threshold.
Speakers questioned after the first press briefing of the
day gave these views pretty short shrift, however.
"Unabated climate change will make it much harder to
eradicate poverty and beyond a certain threshold will make it impossible,"
said John Ashton of the UK Foreign and Commonwealth office.
Ian Chubb of Australian National University added, "As an Australian I think we are very good at looking for British plots and even we can't see one here."
Once the conference kicked off for real, however, the
outlook was more bleak. A wide range of climate and other scientists have come
together to discuss their discoveries since the IPCC report of 2007. Because of
the way that report was produced, that means any results from the last 4-5
years. In a nutshell, the news is not good.
Carbon emissions are now at the upper bound of those
projected by the IPCC, sea level rise could well top one metre by the end of
the century, and it appears that tropical forest carbon sinks are likely to
decline as the planet warms, to name just a few.
"The good news is in the social sciences and the
human sciences," said Katherine Richardson of the University of Copenhagen
and chair of the conference scientific steering committee. "In those
fields you will find we have a lot of tools in our toolbox, things we can do
already."
For once, the credit crunch is arguably good news as it's
likely to see a slowdown in world carbon emissions. Although, according to
Terry Barker of the University of Cambridge, it could also lead to a collapse
of the European emissions trading scheme as declining demand for electricity
leads to a plummeting price for emissions credits.
"Politicians have refocused on jobs because of the
economic crisis," said John Ashton of the UK Foreign and Commonwealth
Office. "If we want a successful response to climate change we have to
reframe it in terms of jobs. We need to build the prospect of a low carbon
recovery."
The plan is for the output from the conference to feed
into the climate negotiations for the follow-on treaty to the Kyoto Protocol to
be held in the same venue in December. "We are looking for things to
happen from this conference, not just more talk," said Ian Chubb of
Australian National University
With that in mind, organizers will produce a 30 page long
synthesis report by June 1st while next year will see the release of a book.
What's more, at the conference closing ceremony on Thursday, Danish prime
minister Anders Fogh Rasmussen will receive a summary of a handful of key
results presented at the event. He'll then discuss these with a panel of
leading researchers, including Dan Kammen of the University of California,
Berkeley, and Nicholas Stern of the London School of Economics and Political
Science. Watch this space for more.
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