View
of Sheldon Glacier with Mount Barre in the background, seen from Ryder Bay near
Rothera Research Station, Adelaide Island, Antarctica. A new NASA/British
Antarctic Survey study examines why Antarctic sea ice cover has increased under
the effects of climate change over the past two decades. Image credit: British
Antarctic Survey.
New survey highlights marked changes in the drift of Antarctic sea ice due to changing wind patterns around the frozen continent. SANDY ANDERSON reports.
The
first direct evidence that marked changes to Antarctic sea ice drift have
occurred over the last 20 years, in response to changing winds, is published
this week in the journal Nature Geoscience. Scientists from the British
Antarctic Survey (BAS) and NASA's Jet Propulsion Laboratory (JPL), Pasadena
California explain why, unlike the dramatic losses reported in the Arctic, the
Antarctic sea ice cover has increased under the effects of climate change.
Maps
created by JPL using over 5 million individual daily ice motion measurements
captured over a period of 19 years by four US Defense Meteorological satellites
show, for the first time, the long-term changes in sea ice drift around
Antarctica.
Lead
author, Dr Paul Holland of BAS says: "Until now these changes in ice drift
were only speculated upon, using computer models of Antarctic winds. This study
of direct satellite observations shows the complexity of climate change. The
total Antarctic sea-ice cover is increasing slowly, but individual regions are actually
experiencing much larger gains and losses that are almost offsetting each other
overall. We now know that these regional changes are caused by changes in the
winds, which in turn affect the ice cover through changes in both ice drift and
air temperature. The changes in ice drift also suggest large changes in the
ocean surrounding Antarctica, which is very sensitive to the cold and salty
water produced by sea-ice growth."
"Sea
ice is constantly on the move; around Antarctica the ice is blown away from the
continent by strong northward winds. Since 1992 this ice drift has changed. In
some areas the export of ice away from Antarctica has doubled, while in others
it has decreased significantly."
Sea
ice plays a key role in the global environment - reflecting heat from the sun
and providing a habitat for marine life. At both poles sea ice cover is at its
minimum during late summer. However, during the winter freeze in Antarctica
this ice cover expands to an area roughly twice the size of Europe. Ranging in
thickness from less than a metre to several metres, the ice insulates the warm
ocean from the frigid atmosphere above.
The
new research also helps explain why observed changes in the amount of sea-ice
cover are so different in the two Polar Regions. The Arctic has experienced
dramatic ice losses in recent decades while the overall ice extent in the
Antarctic has increased slightly. However, this small Antarctic increase is
actually the result of much larger regional increases and decreases, which are
now shown to be caused by wind-driven changes. In places, increased northward
winds have caused the sea-ice cover to expand outwards from Antarctica. The
Arctic Ocean is surrounded by land, so changed winds cannot cause Arctic ice to
expand in the same way.
Dr
Ron Kwok, JPL says, "The Antarctic sea ice cover interacts with the global
climate system very differently than that of the Arctic, and these results
highlight the sensitivity of the Antarctic ice coverage to changes in the
strength of the winds around the continent."
There
has been contrasting climate change observed across the Antarctic in recent
decades. The Antarctic Peninsula has warmed as much as anywhere in the Southern
Hemisphere, while East Antarctica has shown little change or even a small cooling
around the coast. The new research improves understanding of present and future
climate change. It is important to distinguish between the Antarctic Ice Sheet
- glacial ice - which is losing volume, and Antarctic sea ice - frozen seawater
- which is expanding.

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