Press Release
28 September 2005

Sea Ice Decline Intensifies

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Figure 1: September extent trend, 1978-2005. This graph depicts the decline in sea ice extent from 1978-2005. The September trend from 1979 to 2005, now showing a decline of more than 8 percent per decade, is shown with a straight blue line.

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Figure 2: Five-day running mean. This graph shows the daily ice extent in the summers of 2002-2005. The lines dip to a show a minimum extent each September; the lines bend upward as melting slows and fall begins.

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Figure 3: This maps shows the difference between “normal” sea ice extent (long-term mean), and the current year. The long-term average minimum extent contour (1979-2000) is in magenta.

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Figure 4: Melt onset anomaly maps, 2002-2005. This map shows the difference between “normal” timing of spring melting (the long-term mean) and when melting started in the year indicated. Red is sooner and blue is later.

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Figure 5: Surface temperature anomaly. This image shows the difference between 2005 surface air temperatures in degrees Celsius (averaged for January through August) and the fifty-year mean (1955-2004) for the same months. The preponderance of positive values indicates an unusually warm Arctic in 2005. Credit: NCEP/NCAR Reanalysis; NOAA-CIRES Climate Diagnostics Center

For the fourth consecutive year, NSIDC and NASA scientists using satellite data have tracked a stunning reduction in arctic sea ice at the end of the northern summer. The persistence of near-record low extents leads the group to conclude that Arctic sea ice is likely on an accelerating, long-term decline.

“Considering the record low amounts of sea ice this year leading up to the month of September, 2005 will almost certainly surpass 2002 as the lowest amount of ice cover in more than a century,” said Julienne Stroeve of NSIDC. If current rates of decline in sea ice continue, the summertime Arctic could be completely ice-free well before the end of this century. (Figure 1: September extent trend, 1978-2005).

Arctic sea ice extent, or the area of ocean that is covered by at least 15 percent ice, typically reaches its minimum in September, at the end of the summer melt season. On September 21, 2005, the five-day running mean sea ice extent dropped to 5.32 million square kilometers (2.05 million square miles), the lowest extent ever observed during the satellite record (Figures 2 and 3: Five-day running mean).

This record covers the period 1978 to the present. A recent assessment of trends throughout the past century indicates that the current decline also exceeds past low ice periods in the 1930s and 1940s (for figures, see Additional Information, below).

For the period 1979 through 2001, before the recent series of low extents, the rate of September decline was slightly more than 6.5 percent per decade. After the September 2002 minimum, which was the record before this year, the trend steepened to 7.3 percent.

Incorporating the 2005 minimum, with a projection for ice growth in the last few days of September, the estimated decline in end-of-summer Arctic sea ice is now approximately 8 percent per decade. All four years have ice extents approximately 20 percent less than the 1978 through 2000 average. This decline in sea ice amounts to approximately 1.3 million square kilometers (500,000 square miles). This is an area roughly equivalent to twice the size of Texas.

With four consecutive years of low summer ice extent, confidence is strengthening that a long-term decline is underway. Walt Meier of NSIDC said, “Having four years in a row with such low ice extents has never been seen before in the satellite record. It clearly indicates a downward trend, not just a short-term anomaly.”

In addition, however, this year brings with it some new anomalies.

The winter recovery of sea ice extent in the 2004-2005 season was the smallest in the satellite record. Cooler winter temperatures allow the sea ice to “rebound” after summer melting. But with the exception of May 2005, every month since December 2004 has set a new record low ice extent for that month.

Florence Fetterer, of NSIDC, explained how the situation has changed. “Even if sea ice retreated a lot one summer, it would make a comeback the following winter, when temperatures fall well below freezing,” she said. “But in the winter of 2004-2005, sea ice didn't approach the previous wintertime level.” This lack of recovery means that the sea ice is not building back up after a summer of melting—leaving it even more susceptible to warmer summer temperatures.

In mid-September, NSIDC Director Roger Barry spent time in the Laptev Sea on an arctic icebreaker. The ship entered only one area of continuous ice to the east of Severniya Zemvya, one of the most northern island chains of Russia. "That whole area was covered in thick multiyear ice last year, in September of 2004." The Northeast Passage, north of the Siberian coast, was completely ice-free from August 15 through September 28.

Barry mused about the possible effects of the sea ice decline, including the impact on Arctic animals. “We saw several polar bears quite close to the ship,” he said. “Polar bears must wait out the summer melt season on land, using their stored fat until they can return to the ice. But if winter recovery and sea ice extent continue to decline, how will these beasts survive?”

Since 2002, satellite records have also revealed that springtime melting is beginning unusually early in the areas north of Alaska and Siberia. The 2005 melt season arrived even earlier, beating the mean melt onset date by approximately 17 days, this time throughout the Arctic (Figure 4: Melt onset anomaly maps, 2002-2005).

In addition, arctic temperatures have increased in recent decades. Compared to the past 50 years, average surface air temperatures from January through August, 2005, were 2 to 3 degrees Celsius (3.6 to 5.4 degrees Fahrenheit) warmer than average across most of the Arctic Ocean (Figure 5: Surface temperature anomaly).

“The year 2005 puts an exclamation point on the pattern of Arctic warming we’ve seen in recent years,” said Mark Serreze of NSIDC.

“The sea ice cover seems to be rapidly changing and the best explanation for this is rising temperatures,” Serreze said.

The trend in sea ice decline, lack of winter recovery, early onset of spring melting, and warmer-than-average temperatures suggest a system that is trapped in a loop of positive feedbacks, in which responses to inputs into the system cause it to shift even further away from normal.

One of these positive feedbacks centers on increasingly warm temperatures. Serreze explained that as sea ice declines because of warmer temperatures, the loss of ice is likely to lead to still-further ice losses. Sea ice reflects much of the sun's radiation back into space, whereas dark ice-free ocean absorbs more of the sun's energy. As sea ice melts, Earth's overall albedo, the fraction of energy reflected away from the planet, decreases. The increased absorption of energy further warms the planet.

“Feedbacks in the system are starting to take hold,” argues NSIDC Lead Scientist Ted Scambos. Moreover, these feedbacks could change our estimate of the rate of decline of sea ice. “Right now, our projections for the future use a steady linear decline, but when feedbacks are involved the decline is not necessarily steady—it could pick up speed.”

The arctic system is large and complex, and there are many factors driving change in the region. For example, scientists believe that the Arctic Oscillation, a major atmospheric circulation pattern that can push sea ice out of the Arctic, may have contributed to the sea-ice reduction in the mid-1990s. However, the pattern has become less of an influence in the region since the late 1990s, and yet sea ice has continued to decline.

On his arctic cruise, Barry saw another example of a factor that contributes to changes in the Arctic. "Warm water flowing from the Atlantic is persisting in the Siberian arctic in a layer 100 to 400 meters, or 109 to 437 yards, below the surface," Barry said. Heat is probably transferring upward from this layer, helping to maintain open water conditions.

Scientists point out that a longer record of data will continue to help them better examine, piece apart, and understand both the influences and the remarkable changes that they are now seeing.

Scientists who collaborated on this study work at the NASA Goddard Space Flight Center in Greenbelt, Maryland; the NASA Jet Propulsion Laboratory in Pasadena, California; NSIDC at the University of Colorado in Boulder, Colorado; and the University of Washington in Seattle, Washington.

Studies of arctic sea ice extent are funded by NASA and NOAA. In assessing present-day Arctic sea ice extent, researchers used data from NASA, NOAA, U.S. Department of Defense, and Canadian satellites and weather observing stations.

Additional Information

All About Sea Ice
General information, global climate, trends, wildlife, ice development, ice growth, melt, and cycle, remote sensing and modeling

NSIDC Sea Ice Index
Images, animations, and trends (September numbers updated first week of October).

State of the Cryosphere
Overview of sea ice extent and its importance; content last updated March 2005.

Arctic Climate Impact Assessment (ACIA)
Visit the ACIA site to view graphics and explanations about sea ice in Impacts of a Warming Arctic report.

Changes in other areas: Greenland Melt Extent, 2005

Further Reading
Meier, W., J. Stroeve, F. Fetterer, and K. Knowles. 2005. Reductions in Arctic sea ice cover no longer limited to summer. EOS 86:326-327.

Overpeck, J., M. Sturm, J. Francis, D. Perovich, et al. 2005. Arctic system on trajectory to new, seasonally ice-free state. EOS 86:309-313.

Serreze, M.C., and J.A. Francis. 2005. The Arctic amplification debate. Climatic Change, in press.

Lindsay, R.W., and J. Zhang. 2005. The thinning of Arctic sea ice, 1988-2003: Have we passed a tipping point? Journal of Climate, in press.

Stroeve, J., M.C. Serreze, F. Fetterer, T. Arbetter, W. Meier, J. Maslanik, K. Knowles. 2005. Tracking the Arctic's shrinking ice cover; another extreme September sea ice minimum in 2004. Geophysical Research Letters, 32, L04501, doi:10.1029/2004GL021810.

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