New Delhi: New
research led by the University of Washington (UW) shows that even in their
quiet phases volcanoes release at least three times as much sulphur into the
Arctic atmosphere than estimated by current climate models. The study’s
findings, which were published in a recent issue of Geophysical
Research Letters, have implications for scientists’ understanding of the
atmosphere and its relationship with climate and air quality.
photo :Google image
Layers of a central Greenland ice core
were analysed to calculate levels of sulphate aerosols between the years 1200
and 1850. The authors had wanted to look at the sulphur emitted by marine
phytoplankton, which were believed to be the biggest source of atmospheric
sulphate in pre-industrial times.
The team focussed on this time period as it avoids major volcanic
eruptions and makes it easier to distinguish between volcanic and marine
sources. “We don’t know what the natural, pristine atmosphere looks like, in
terms of aerosols,” said senior author Becky Alexander, a UW professor.
“Knowing that is a first step to better understanding how humans have
influenced our atmosphere.”
“We were planning to calculate the amount of sulphate coming out of
volcanoes, subtract it, and move on to study marine phytoplankton,” said Ursula
Jongebloed of UW, the first author of the paper. “But when I first calculated
the amount from volcanoes, we decided that we needed to stop and address that.”
“We found that on longer timescales the amount of sulphate aerosols
released during passive degassing is much higher than during eruptions,” she
said. “Passive degassing releases at least 10 times more sulphur into the
atmosphere, on decadal timescales, than eruptions, and it could be as much as
30 times more.”
“Our results suggest that volcanoes, even in the absence of major
eruptions, are twice as important as marine phytoplankton,” Jongebloed said.
Aerosol particles, whether from volcanoes, automobiles, factory
chimneys, or firewood burning, block some solar energy. If the natural levels
of aerosols are higher, that means the rise and fall of emissions caused by
humans have had less of an effect on temperature than previously believed.
“When we increase volcanic emissions, which increase the baseline of sulphate
aerosols, we decrease the effect that the human-made aerosols have on the
climate by up to a factor of two,” Jongebloed said. That can improve global
climate models.
@frontline
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