Dec 16 2007
Arctic Summer Melting in 2007 Set New Records
San Francisco, Calif — Arctic sea ice shrank drastically this summer, reaching a record low, largely because warm ocean currents ate away at the base of the ice sheet, new research says. The arctic ice cap melted at an unprecedented rate in mid-2007, losing an area of ice the size of the state of Alaska, US scientists said at a conference this week.
“The average rate of loss of sea ice every summer year to year up to 2006 was equal to an area the size of West Virginia,” or about 62,800 square kilometers (24,250 square miles), said Michael Steele, the senior oceanographer at the University of Washington in Seattle.
However the decrease in ice between 2006 and 2007 “was almost equivalent to the area of Alaska,” or some 1.7 million kilometers (more than 663,000 square miles), Steele further said.
“It was a huge retreat,” said Steele, one of the researchers who discussed the subject at the annual American Geophysical Union (AGU) conference in San Francisco, California.
At the fall meeting of the American Geophysical Union (AGU) in San Francisco, some scientists argued yesterday that the end of the perennial ice is near.
“If this trend persists, the Arctic would be ice-free [in the summer] by 2013,” said Wieslaw Maslowski of the Naval Postgraduate School in Monterey, California. The researchers told a meeting of the American Geophysical Union that some of the observations had been astonishing.
“The further you go down this path, the harder it is to get back,” observed Don Perovich from the US Army Cold Regions Research and Engineering Laboratory. “Things could come back, but basically it’s the fourth quarter and we’re down two touchdowns,” he said, using an analogy from American football.
The big thin
The extent of the sea ice cover fell to a record minimum in September of 4.13 million sq km, beating the previous low mark, set in 2005, by 23%. This was well publicised at the time, but some of the other “Arctic numbers” have not been so widely reported. Scientists say they demonstrate the step changes in environmental conditions in the northern polar region.
Warmth from below
A big driver behind the melt is the current warmth of the waters in the Arctic. In the summer of 2007, Arctic Ocean surface temperatures hit new maximums.
In waters just north of the Chukchi Sea (above Alaska and Eastern Siberia), sea-surface temperatures (SSTs) were 3.5C warmer than the historical average and 1.5C warmer than the historical maximum. SSTs of 4C were recorded.
This warming was probably the result of having increasing amounts of open water that readily absorb the sun’s rays, a phenomenon known as the ice-albedo feedback: less ice means less reflection and more absorption, leading to more warming and more melting.
“Water that is now circulating just 200 meters below the main ice pack is now significantly warmer than it was just five years ago,” said John Walsh of the University of Alaska, Fairbanks.
New research shows that carbon dioxide, one gas that traps heat in the atmosphere, can be captured as it leaves coal-burning power plants and then permanently sequestered in rock formations thousands of feet below the Earth’s surface.
How Much Time Is Left?
When asked how long the perennial ice might last, many researchers here shrugged their shoulders.
A report from the Intergovernmental Panel on Climate Change released in February predicts that the summer sea ice may disappear early in the next century.
More at National Snow and Ice Data Center, BBC News.
September 9, 2007, sea ice extent compared to animation of Septembers 1979 to 2006











