Vicious
Global Warming Feedback Loop Worse Than Feared
Vicious
cycle: amount of warming involved in Arctic ice loss, now amounts to
roughly one-quarter of all warming
-
Jacob Chamberlain, staff writer
19
February, 2014
One
of nature's key defenses against global warming—the reflection of
the sun's rays away from Earth by Arctic sea ice—has fallen victim
to... global warming. And according
to a study published
Monday, the vicious feedback loop is worse than previously thought.
The
new research, published in the Proceedings
of the National Academy of Sciences,
shows the ability of the Arctic ice to reflect sunlight—known
scientifically as albedo—hasdecreased
dramatically since 1979,
with the calculations showing the region's ability to reflect
sunlight diminished more than twice what previous studies have shown.
As
less of the sun's rays are reflected back into space, the open ocean
absorbs more heat leading to additional ice melt in the region. The
problem is both self-feeding and a source of deep concern for
scientists and those concerned about climate change.
"That
is big – unexpectedly big," said
the study's lead author Ian
Eisenman, a climate scientist at the Scripps Institution of
Oceanography in California, on the rate of loss. "Arctic sea ice
retreat has been an important player in the global warming that we've
observed during recent decades."
And
Mark Flanner, a climate researcher at the University of
Michigan, told the New
Scientistthat
the study "reaffirms that albedo feedback is a powerful
amplifier of climate change, maybe even more so than is simulated by
the current crop of climate models."
The report is
the first to use satellite measurements dating back to 1979 to gauge
decreasing sunlight reflection in the region.
The
amount of Arctic warming caused by this phenomenon now amounts to
roughly one-quarter of the total warming caused by the greenhouse
effect, said the researchers.
"Basically,
it means more warming," said Eisenman.
The Arctic sea ice retreat has been one of the most dramatic climate changes in recent decades. Nearly 50 years ago it was predicted that a darkening of the Arctic associated with disappearing ice would be a consequence of global warming. Using satellite measurements, this analysis directly quantifies how much the Arctic as viewed from space has darkened in response to the recent sea ice retreat. We find that this decline has caused 6.4 ± 0.9 W/m2 of radiative heating since 1979, considerably larger than expectations from models and recent less direct estimates. Averaged globally, this albedo change is equivalent to 25% of the direct forcing from CO2 during the past 30 years.
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