All in all, she placed nearly 70,000 such points on the photos. It took the better part of two years. “I started to have to wear these glasses, I think,” she said, pointing at her face, “because of squinting so much at pixelated images on my screen.”
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In some places, fresh white snow in the photos made it too hard to make out the terrain, so she filled in the gaps with estimates.
Once they had digital reconstructions of more than 1,500 glaciers across Svalbard, Ms. Geyman and her co-authors compared them with ones made from more recent images to determine how much the ice had melted since the 1930s.
They then used these specifications to predict that the average elevation of Svalbard’s glaciers would shrink by between 2.2 and 3 feet a year before 2100, depending on the increase of greenhouse gases in the atmosphere. Those rates are at least 1.9 times the pace of retreat that occurred in the 20th century, even in a modest warming scenario in which global temperature increases are limited to 2 degrees Celsius (3.6 degrees Fahrenheit) above preindustrial levels.
Researchers have been creating three-dimensional computer models of individual glaciers for several years now. But only recently have increases in processing power made it feasible to reconstruct ice sheets across entire regions and mountain ranges, said Erik S. Mannerfelt, a glaciologist at the Swiss university ETH Zurich who did not work on the new study.
“This is a new era where we can look not at individual glaciers, but at populations” of them, he said.
Mr. Mannerfelt is finishing a separate paper that uses 22,000 photos taken by Swiss mountaineers between the two world wars to capture changes in Switzerland’s glaciers since the early 1930s. He hopes that other image archives might enable similarly detailed reconstructions of the ice in South America’s Tierra del Fuego islands and in the Himalayas.