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Seeing Greenland

New imaging technique shows how fast inland ice is melting.
March 1, 2007

There’s enough frozen water in Greenland to raise global sea levels seven meters, and enough in Antarctica to raise levels 65 meters. But the rate of melting is poorly understood, partly because ice-sheet surfaces look so inscrutably white and featureless in ordinary satellite images and to the human eye. Now, a new image-­processing technique gives a clearer view of critical features of inland ice.

Thanks to new image processing technology, fine-grained features of ice flow are visible within this eyedropper-shaped 600-by-50-kilometer ice formation in Greenland.

The technology starts with as many as 94 red and infrared images of the same region, taken by two NASA satellites, Terra and Aqua, with orbits that cross Greenland several times a day. By aligning and averaging values within areas of pixel overlap, researchers tightened resolution from 250 meters per pixel to as little as 150 meters, says Ted ­Scambos, the lead scientist and glaciologist at the National Snow and Ice Data Center at the University of Colorado at Boulder, who was one of the developers. The new approach also allows rapid reëvalua­tion of the entire ice sheet overlying Greenland to detect important short-term changes. “What we’ve got is a map that shows details much further inland, much better than before,” says Scambos. “Other images just show the interior of the ice sheet as a blank white surface.” Mark ­Fahnestock, a geologist at the University of New Hampshire in Durham who collaborated with ­Scambos, says the technology is key to understanding today’s accelerating ice-sheet melting.

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