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Last update - 20:19 02/09/2007
Greenland's ice sheet still flows to the sea - as water
By Assaf Uni, Haaretz Correspondent

ILULISSAT, Greenland - As in every summer for the past 20 years, Konrad Steffen spent this past one high atop Greenland's ice sheet. In 1990, the University of Colorado at Boulder professor, one of the world's greatest experts on climate change, established a project known as Swiss Camp, where research is conducted into the changing nature of the Greenland ice sheet. And changing it certainly is, for the worse.

"The situation is deteriorating from year to year," Steffen says during an interview at the airport of this small town, some 250 kilometers north of the Arctic Circle. "We set up the camp in 1990 at an altitude where there should not have been any melting. But this summer alone, the camp lost an entire meter in altitude as a result of melting ice. If you double that by the area of the entire ice cap, you get an awful lot of water. "We never had anything like this," adds Steffen, who is tall and thin, with an overgrown blond beard.

"We lost equipment that disappeared in the water, we discovered huge slits that formed beneath the ice. In fact, the ice cap is losing so much ice that the camp itself has begun to come apart. Next year I think I'll have to rebuild it."

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Massive melting of this scale, he says, can raise the sea level sharply in the coming decades. If you go up in a hot-air balloon over the North Pole, with your backs to the Siberian Tundra and facing North America, what you'll see in front of you will be mainly ice sea. On the right will be the permafrost Arctic sea, a silent ocean surrounded by distant continents, where temperatures plunge to 40 degrees below zero in winter. But if you guide the balloon to your left, you can spot in front of you a giant body rising sharply above the frozen sea; an enormous white mass in the distance, whose front stretches along hundreds of kilometers, rising to heights of 3,000 meters, and continuing to the horizon. That is Greenland. The largest island in the world, the closest land mass to the North Pole. Almost this entire mass, which stretches over an area of 2.2 million square kilometers, has a depth of 3 kilometers on average and a volume about half that of the Mediterranean, is one big chunk of ice, made of sweet water.

About 8 percent of the ice in the world is concentrated in Greenland's ice cap, which overlies the island's granite ground. To a great extent, it is a remnant of the glaciation process the earth underwent 125,000 years ago, when its northern half was covered with ice layers kilometers deep. Besides its proximity to the North pole, the central reason why the Greenland ice sheet survived has to do with its dimensions. It's so big that it has its own climate.

Here in Ilulissat, on the island's exposed western edges, one can see how the process occurs. The town, with a population of 3,700, is located at the northern mouth of the Jakobshavn Glacier, the northern hemisphere's most fertile ice fjord. For tens of thousands of years it's acted as a sort of valve for part of the Greenland ice sheet: At one end, ancient ice is shoved into it, and at the other, ice is released into the sea in enormous pieces.

Across from the town's homes is a field of huge glaciers, like prehistoric animals wallowing in the water, slowly melting and making their way to the Atlantic. The water fills the air with vapor, which collects over the island and turns into snow clouds over central Greenland. There, over the years, the snow turns into packed ice, and flows like water, only much more slowly, toward the Jakobshavn Glacier, to begin the process again.

But something has changed in recent years. The balance has been broken. The glaciers' melting pace became higher than the rate of snowfall in the island's center. In each of the past few years, Greenland lost an amount of water equal to that contained in the entire Alpine range. And the snow falling in its center cannot make up for that. In addition, Steffen and his colleagues have taken a series of unusual measurements, which point to climate change. Air temperature in the Greenland winter has gone up four degrees, the sharpest increase anywhere in the world; the rate of glacier movement to the sea has doubled; and the ice sheet itself has begun oozing ever-faster westward toward the sea, sliding on melted water that acts as lubricant.

"After this summer, we reached one conclusion," Steffen said, "Greenland is melting." This has climate researchers worried, because Greenland, they say, is like a canary in a coal mine: If it dies, then so does the earth.
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