Potsdam, 09/09/1999
A new study of the possible effects of global warming
in the coming millennium is presented this week by scientists of the Potsdam
Institute for Climate Impact Research. The study adds further credibility
to fears that the global temperature could rise by over 3°C by the
end of the next century if greenhouse gas emissions continue unabated.
It also investigates the risk of a major lasting ocean circulation change
in response to the warming.
Stefan Rahmstorf and Andrey Ganopolski used a computer
model developed for long-term climate simulations at the Potsdam Institute.
In contrast to previous climate models, their model has been tested by
reproducing major climatic changes of the past. Last year, the Potsdam
team was the first to succeed in a realistic simulation of the climate
at the height of the last Ice Age, 21,000 years before present (Nature,
22 January 1988). And in July this year, the team headed by Martin Claussen
again grabbed the headlines when their model showed how the Sahara had
turned into a desert 5,500 years ago (Geophysical Research Letters, 15
July 1999). Other periods in the climate history were also simulated with
the same model, such as the Eemian interglacial (warm period) that preceeded
the last Ice Age.
The fact that most climate models have never been tested
on past climatic changes has often been used by critics to question their
reliability for the future. The model developed in Potsdam is coarser but
runs much faster than previous models, which allows the simulation of tens
of thousands of years of climate history.
"When we saw that our model can get past climates right
we turned it to the future," says Ganopolski. "We used a new kind of model
with a radically different approach, we tested it thoroughly on past climates,
and we still get the same kind of warming in the next century as other
studies. That strengthens the case for global warming." The model results
for the next century are consistent with the assessment of the Intergovernmental
Panel on Climate Change (IPCC), which advises the world's governments on
climate issues.
Going beyond most previous scenarios, the new study looks
at possible climate changes up to a thousand years into the future. It
demonstrates for the first time how global warming could eventually lead
to a lasting cooling of Europe if the North Atlantic ocean circulation
collapses. Such a cooling has been the focus of much speculation, but had
not previously been shown in a computer simulation. "We can't yet say how
likely this is, but it is a possibility," says Rahmstorf. "Our results
show that this depends on changes in the atmospheric water cycle which
are still difficult to predict."
The study is published this week in the journal Climatic
Change (Vol. 43 Nr. 2, pp. 353-367) and presented at the International
Conference on Modelling of Global Climate Change and Variability in Hamburg
(13.-17. Sept.).
The study is available at: http://www.pik-potsdam.de/~stefan/
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