090129: "Clean Air" in Europe Causes "Warming"
January 19, 2009
Paris (AFP) - Fog, mist and haze in Europe have declined over the last three
decades, a trend that may have stoked regional warming, a recent study
concludes.
From 1978-2006, temperatures in parts of Europe rose above the global land
average, with prominent increases in the north, center and eastern parts of the
continent.
As much as 20 percent of Europe's warming during this time, according to the
study, can be pinned on a reduction in fog, mist and haze, which -- because they
are white -- reflect solar radiation and thus keep the ground cool.
In eastern Europe, the decline in fog, mist and haze could account for 50
percent, the study believes.
The authors, led by Robert Vautard of France's Atomic Energy Commission
(CEA), pored over data from 342 weather stations around Europe.
They found that over nearly 30 years, the number of days categorized as
having restricted visibility fell by half. These categories were determined by
ranges of visibility at two kilometres (1.2 miles), five kms (three miles) and
eight kms (five miles).
The phenomenon is closely linked to falling levels of atmospheric sulphur
dioxide (S02), a byproduct of burning oil and coal that causes notorious "acid
rain" that damages forests and lakes.
The temperature rise has been especially perceptible in Eastern Europe,
where the end of the Communist system closed down innumerable sources of coal
pollution.
However, the SO2 cleanup is now largely tapering off.
This means the fog reduction will probably stop and "the warming trend in
Europe will not be so large in the coming years," Vautard told AFP.
According to the Intergovernmental Panel on Climate Change (IPCC) -- the
UN's paramount authority on global warming -- the global average temperature
rose 0.74 degrees Celsius (1.33 degrees Fahrenheit) from 1906-2005, and the pace
in the last 50 years was double that of the first half-century.
A blanket of fog can reduce local temperatures by some 2 C (3.6 F),
according to figures quoted in the new study.
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