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Arctic sea ice rebounds, but don't jump to 'global cooling' conclusions

Parts of the Arctic Ocean containing at least 15 percent sea ice have increased by 78 percent when compared with the extent last year at this time, according to data compiled by the National Snow and Ice Data Center.

By Staff writer / September 10, 2013

The crew of the US Coast Guard Cutter Healy, in the midst of their ICESCAPE mission, retrieves supplies for some mid-mission fixes dropped by parachute from a C-130 in the Arctic Ocean on July 12, 2011.

Kathryn Hansen/NASA/Reuters/File


After a record-breaking decline in the extent of summer sea ice on the Arctic Ocean last year, this year's minimum has returned to levels that more closely track the long-term rate of decline that scientists have measured for at least 34 years.

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The striking one-year recovery in end-of-melt-season ice speaks more to the role that natural variability plays in any single year's number, Arctic sea-ice specialists say. It says little or nothing about any purported global cooling, as some skeptics of climate change have suggested.

Researchers note that the long-term decline in summer sea ice is strongly correlated with rising temperatures in the region, increases they attribute to global warming.

Scientists are keeping close tabs on Arctic sea ice because it plays an important role in the global climate in general and Northern Hemisphere climate in particular. During the summer, when the Arctic landscape is absorbing sunlight and re-radiating it as heat, Arctic sea ice acts as a counterweight. Its white surface reflects sunlight back into space, keeping the region cooler than it might otherwise be.

As summer sea ice declines, sunlight reaches ever-larger patches of ocean to be absorbed and converted to heat. This amplifies the warming that the region experiences. That warming in turn can alter atmospheric circulation patterns at lower latitudes.

Exactly how that happens is still an open question. The National Research Council is sponsoring a meeting on the topic at the University of Maryland in College Park Thursday and Friday. Scientists exploring the issue are slated to review the latest thinking on a warming Arctic's broader atmospheric reach and to try to outline a research agenda to fill gaps in that knowledge.

This year's recovery in summer sea ice at the top of the world is dramatic. On Sept. 16, 2012, parts of the Arctic Ocean containing at least 15 percent sea ice dropped to a record low of 1.32 million square miles.

As of Sept. 9, 2013, sea-ice extent covered 2.35 million square miles of Arctic Ocean, according to data compiled by the National Snow and Ice Data Center in Boulder, Colo. That puts 78 percent more ice on the ocean this month than at the same time last year.

The melt season is not over yet, but typically ends in mid-September.

Despite the impressive one-year recovery, the current sea-ice extent is still nearly 400,000 square miles below the 1981-2010 average minimum. Through August, the long-term decline since 1979, when satellites first began tracking sea-ice extent, has been running at 10.6 percent per decade.

Large portions of the Arctic Ocean remain essentially ice-free. Areas covered by at least 15 percent sea ice are still clinging to the Arctic coast from northern Greenland west through much of the Canadian archipelago.


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