Last September, at the end of the northern hemisphere summer, the Arctic Ocean’s
icy cover shrank to its lowest extent on record, continuing a long-term trend
and diminishing to about half the size of the average summertime extent from
1979 to 2000.
During the cold and dark of Arctic winter, sea ice
refreezes and achieves its maximum extent, usually in late February or early
March. According to a NASA analysis, this year the annual maximum extent was
reached on Feb. 28 and it was the fifth lowest sea ice winter extent in the past
35 years.
The new maximum —5.82 million square miles (15.09 million
square kilometers)— is in line with a continuing trend in declining winter
Arctic sea ice extent: nine of the ten smallest recorded maximums have occurred
during the last decade. The 2013 winter extent is 144,402 square miles (374,000
square kilometers) below the average annual maximum extent for the last three
decades.
"The Arctic region is in darkness during winter and the
predominant type of radiation is long-wave or infrared, which is associated with
greenhouse warming," said Joey Comiso, senior scientist at NASA Goddard Space
Flight Center, Greenbelt, Md., and a principal investigator of NASA’s
Cryospheric Sciences Program. "A decline in the sea ice cover in winter is thus
a manifestation of the effect of the increasing greenhouse gases on sea
ice."
Satellite data retrieved since the late 1970s show that sea ice
extent, which includes all areas of the Arctic Ocean where ice covers at least
15 percent of the ocean surface, is diminishing. This decline is occurring at a
much faster pace in the summer than in the winter; in fact, some models predict
that the Arctic Ocean could be ice-free in the summer in just a few
decades.
The behavior of the winter sea ice maximum is not necessarily
predictive of the following melt season. The record shows there are times when
an unusually large maximum is followed by an unusually low minimum, and vice
versa.
"You would think the two should be related, because if you have
extensive maximum, that means you had an unusually cold winter and that the ice
would have grown thicker than normal. And you would expect thicker ice to be
more difficult to melt in the summer," Comiso said. "But it isn’t as simple as
that. You can have a lot of other forces that affect the ice cover in the
summer, like the strong storm we got in August last year, which split a huge
segment of ice that then got transported south to warmer waters, where it
melted."
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