January 14, 1986 Retreat of the Sierra de Sangra Glaciers
January 14, 2015 Retreat of the Sierra de Sangra Glaciers
acquired January 14, 1986 download large image (4 MB, JPEG, 2000x3000 - left)
acquired January 14, 1986 download GeoTIFF file (14 MB, TIFF, 2000x3000)
acquired January 14, 2015 download large image (5 MB, JPEG, 2000x3000 - right)
acquired January 14, 2015 download GeoTIFF file (14 MB, TIFF, 2000x3000)
acquired 1986 - 2015 download Google Earth file (KML)
Retreat of the Sierra de Sangra Glaciers
acquired January 14, 1986 download large image (4 MB, JPEG, 2000x3000)
acquired January 14, 1986 download GeoTIFF file (14 MB, TIFF, 2000x3000)
Retreat of the Sierra de Sangra Glaciers
acquired January 14, 2015 download large image (5 MB, JPEG, 2000x3000)
acquired January 14, 2015 download GeoTIFF file (14 MB, TIFF, 2000x3000)
acquired 1986 - 2015 download Google Earth file (KML)

Since the end of the Little Ice Age, the ice fields of Patagonia and other parts of South America have been shrinking as global temperatures have increased. A number of studies have investigated these changes, which can affect the communities downstream that rely on the glaciers for a steady water supply.

“The focus is usually on the bigger ice fields, such as the Northern Patagonia ice field, the Southern Patagonia ice field, and on tropical glaciers,” said Mauri Pelto, a glaciologist at Nichols College. Many researchers focus on the larger ice fields because they have seen a larger mass loss.

But melting ice is not limited to the largest and most frequently studied ice fields. One example is Patagonia’s Sierra de Sangra—an icy stratovolcano spanning the border of Chile and Argentina, about 50 kilometers east of the Southern Patagonia ice field. The glaciers of Sierra de Sangra cover about 270 square kilometers of land (compared to 13220 square kilometers for the Southern Patagonia ice field).

Pelto decided to look at glaciers in Argentina “primarily because there is less information on them.” First he considered the areas most likely to show visual change, which often occurs in the vicinity of lakes; glaciers that terminate in water lose ice not only from their surface, but also through calving. By comparing imagery from Landsat satellites, he found that the glaciers of Sierra de Sangra are retreating.

The top image, acquired by the Thematic Mapper on Landsat 5, shows the glaciers of Sierra de Sangra on January 14, 1986. The second image, acquired by the Operational Land Imager (OLI) on Landsat 8 shows the area on January 14, 2015. Snow and ice are blue in these false-color images, which use different wavelengths to better differentiate areas of ice, rock, and vegetation. Turn on the image comparison tool to see the glaciers retreat.

“The glaciers are not as large as those of the bigger ice fields,” Pelto said. “Retreat is less in terms of distance, but not in terms of percent of glacier length.” Of the four glaciers that he examined, the southeast outlet glacier retreated the most—about 1200 meters (4,000 feet), or 25 percent of its length. The north outlet retreated by about 700 meters (20 percent); the south outlet by 700 meters (10 percent); and the east outlet by 300 meters (5 percent).

“The changes on the four glaciers in comparison to their overall length are equal to or larger than those of the Northern and Southern Patagonia ice fields,” Pelto said. For comparison, the San Quintin and Steffen glaciers of the Northern Patagonia ice field lost 7 and 12 percent of their lengths, respectively.

For more information about the area, read Pelto’s original blog post here.

NASA Earth Observatory images by Jesse Allen, using Landsat data from the U.S. Geological Survey. Caption by Kathryn Hansen.

Instrument(s): 
Landsat 5 - TM
Landsat 8 - OLI

Retreat of the Sierra de Sangra Glaciers

February 23, 2016
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