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Monday, 9 December, 2002, 12:34 GMT
Record ice loss in Arctic
![]() Satellites have tracked the retreat of perennial sea ice in the Arctic
Greenland's unusual summer slush was part of a record-breaking year of northern polar ice loss, reported by Dr Steffen and other scientists this weekend at the American Geophysical Union (AGU) conference in San Francisco. According to scientists, surface melt on Greenland was the highest in recorded history - and extended to elevations previously untouched by melt - while the amount of Arctic sea ice also reached a record low. While some of the accelerated melting appears to be linked to natural atmospheric oscillations, human influence could not be ruled out, said the scientists. Glacier 'lubrication' Greenland glacier and sea ice melt, combined with disappearing permafrost, the northern expansion of vegetation, and increased fresh water run-off present a "compelling case that something is going on," said Larry Hinzman, of the University of Alaska, Fairbanks.
Such melting encourages further ice loss. The excess water weight pushes down on the glacier at the same time that water seeps through cracks to the underside. The combination accelerates the glacier's flow to the sea. Dr Steffen attributes the increased melt to an unusual low-pressure system that "came earlier and stayed longer" on the island to create unseasonable warm temperatures. Ozone depletion Such a low-pressure system is characteristic of the Arctic Oscillation, an atmospheric sea-sawing that produces warm weather and is also partly responsible for this year's dramatic Arctic sea ice melt, according to Mark Serreze, a researcher at the National Snow and Ice Data Center in Boulder, Colorado.
"The Arctic Oscillation can't explain everything," said Dr Serreze. To what extent these may be human-induced changes is very difficult to say, and Arctic Oscillation itself is subject to human influence, he said. Stratospheric ozone depletion can exacerbate the system by cooling the upper atmosphere, which in turn changes wind and ocean circulation patterns. Dr Serreze suspects that just such an aberrant Arctic Oscillation was behind unusual circulation patterns last winter that weakened sea ice. Positive feedback Changes in the winter wind field broke up floating sea ice to create cracks that suggest the "opening of a Venetian blind," said Dr Serreze. The breaks in the ice allow it to absorb more solar radiation. This triggered an early spring melt, which made the ice vulnerable to the impact of high summer temperatures. "It was like a one-two punch," said Dr Serreze. The loss of Arctic sea ice is "big news", according to University of Alaska, Fairbanks, researcher Larry Hinzman. "Polar sea ice has an important function in moderating the global energy balance," he said. He explained that sea ice has albedo of 0.8. That is, it reflects 80% of the solar radiation. When the sea ice melts you have water, which has an albedo of 0.2. "The sea ice goes from absorbing 20% of solar radiation to absorbing 80%," said Dr Hinzman. This creates positive feedback for further warming. In total, the arctic warming is an unprecedented trend, according to Dr Hinzman. "We're experiencing the most rapid increase in temperature in recorded history," he said.
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