Arctic, Antarctic: Poles Apart
in Climate Response
May 2, 2008
NOAA-While the Arctic and the
Antarctic experience similar greenhouse gas levels and solar
radiation, each region responds in a dramatically different way,
especially in temperature and loss of sea ice, says an international
team of scientists that includes a NOAA oceanographer. While the
Arctic is warming, most of Antarctica is not, largely because of the
ozone hole, but projections indicate that is likely to change.
“While some people would say
this is a paradox, these different responses are mostly consistent
with what we know about how the climate system works,” said James
Overland, lead author and an oceanographer at NOAA’s
Pacific Marine Environmental Laboratory in Seattle.
The findings, based on an
October 2007 polar climate workshop, will be published in the May 6
issue of EOS, a publication of the American Geophysical
Union. Co-authors are John Turner and Gareth Marshall of the British
Antarctic Survey, Jennifer Francis of Rutgers University, Nathan
Gillett of the University of East Anglia, and Michael Tjernstrom of
Stockholm University.
Thirty scientists attended the
Seattle workshop that looked at the Polar Regions from 1987 to 2007.
The scientists concluded, based on new research since the 2007
Intergovernmental Panel on Climate Change Report, that a combination
of factors is responsible for the recent dramatic sea ice loss in the
Arctic as well as masking some of the effects in the Antarctic.
Temperature
- Arctic:
Experienced seasonal temperatures that at times were more than
four degrees Fahrenheit
warmer than usual.
- Antarctic:
For most of the Antarctic, temperatures were not unusual, except
on the Antarctic Peninsula, a finger of land and ice about 1,000
miles south of the tip of South America, which had the largest
increase in temperatures of any location in the Southern
Hemisphere. Temperatures warmed by three degrees Fahrenheit.
Warming temperatures and exposure to ocean waves were cited by the
National Snow and Ice Data Center as the cause of the collapse of
a 160-square-mile segment of the Wilkins Ice Shelf on the
Antarctic Peninsula, which began collapsing in late February.
Sea Ice
- Arctic:
Summer sea ice loss was greater and declining more rapidly than
climate models projected.
- Antarctic: The
amount and stability of the sea ice was not unusual.
Human-Influenced Change
- Arctic: There
are multiple causes for change.
“In the Arctic, there is a
combination of factors, such as warming of the air because of more
greenhouse gases, an unusual wind pattern, and warming of the ocean
water in regions with reduced sea ice,” said Overland.
- Antarctic: Story
is clearer.
Gillett, a climate dynamics
scientist, said, “In the Antarctic, the changes in winds and
temperatures are consistent with how we would expect them to respond
to increased greenhouse gases and depletion of stratospheric
ozone.”
The depletion of ozone has
strengthened the atmospheric circulation, called the Southern Annual
Mode, or SAM. As the ozone hole recovers, the winds that currently
whiz around Antarctica and block air masses from crossing into the
continent’s interior would weaken, and Antarctica would no longer
be so isolated from global warming patterns.
The Future
- Arctic: Sea
ice losses will continue. The study says that a combination of
factors has sent the Arctic into a new state of sea ice loss,
which is occurring much earlier than projected by climate models
subject to greenhouse gases alone.
“Additional warming of
the ocean and an overall thinning of the sea ice makes it difficult
for the Arctic to now return to earlier conditions,” says
Overland.
- Antarctic:
Scientists project that the ozone hole should fully recover by
2070.
“As the ozone hole recovers, we expect that warming will appear
on the central plateau of Antarctica and we will see a reduction
in sea ice area,” said Turner.
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