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For the most recent updates on Arctic sea ice, see Arctic Sea Ice News & Analysis at http://nsidc.org/arcticseaicenews/.

5 April 2006

Winter Sea Ice Fails to Recover,
Down to Record Low

Figure 1. March 2006 mean sea ice extent, indicated by the red dot, is 300,000 square kilometers (115,860 square miles) less than the 2005 record, and 1.2 million square kilometers (463,000 square miles) below the 1979-2000 mean. High-resolution version
graph showing March maximums from 1979-2006, with 2006 well below the mean

Scientists at NSIDC announced that March 2006 shows the lowest Arctic winter sea ice extent since the beginning of the satellite record in 1979 (see Figures 1 and 2). Sea ice extent, or the area of ocean that is covered by at least 15 percent ice, was 14.5 million square kilometers (5.60 million square miles) for this March, as compared to 14.8 million square kilometers (5.72 million square miles) for March 2005, the previous record.

The Arctic sea ice shrinks during the summer and grows, or recovers, during the winter. The ice reaches its maximum extent during March, with a long-term (1979-2000) monthly mean extent of 15.7 million square kilometers (6.06 million square miles). Winter sea ice extent has begun to show a significant downward trend over the past four years.

However, the winter recovery trend is not as striking as the sea ice minimum trend (see the press release Sea Ice Decline Intensifies, 28 September 2005). Changes in the sea ice minimum extent are especially important because more of the sun's energy reaches Earth's surface during the Arctic summer than during the Arctic winter. Sea ice reflects much of the sun's radiation back into space, whereas dark ice-free ocean water absorbs more of the sun's energy. So, reduced sea ice during the sunnier summer months has more of an impact on the Arctic's overall energy balance than reduced ice in the winter.

The lower winter extents are still important, however, because they reflect the pattern of reduced sea ice that scientists have already seen. Low winter recovery means that the ice is freezing up later in the fall and growing at a slower pace in the winter.

Figure 2. The pink line indicates the 1979-2000 mean sea ice extent in winter; current ice extent is indicated by the solid off-white area inside the pink line. Land masses are in green; water is in dark blue. Source: NSIDC Sea Ice Index. High-resolution version
Image shows current sea ice as compared to 1979-2000 mean edge

Walt Meier of NSIDC notes, "Poor winter recovery of the sea ice leads to less new ice growth and thinner ice. The weaker the ice at the end of winter, the more easily it melts the following summer."

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Additional Information

All About Sea Ice
General information about sea ice
Global climate, trends, wildlife
Ice development
Ice growth, melt, and cycle
Remote sensing and modeling

NSIDC Sea Ice Index
Images, animations, and trends

2005 Winter Sea Ice Recovery News Release
Arctic Ice Decline in Summer and Winter

2005 Summer Sea Ice Minimum Press Release
Sea Ice Decline Intensifies