acquired August 22, 1987
acquired August 13, 2013
Retreat of Novatak and East Novatak Glacier
- Landsat 5 - TM
- Landsat 8 - OLI
- Data Date: August 22, 1987 - August 13, 2013
- Visualization Date: August 11, 2014
There are few people around to notice, but the ice in the Brabazon Range is changing rapidly—at least on the time scale of a glacier. Novatak and East Novatak glaciers, located just a few kilometers apart near the outlet of the Alsek River, are two of many retreating glaciers in southeastern Alaska. Over the last 25-years, the ends of Novatak and East Novatak have each retreated by more than a kilometer.
Snowfall in higher-elevation accumulation zones feed both glaciers. Over time, fresh snow compresses into ice that slides through alpine valleys and into a low-lying plain north of the Alsek. Meltwater collects near the ends of the glaciers, forming a sizable proglacial lake. This lake, filled with opaque, light-blue water, is drained by small streams that connect to the Alsek River a few kilometers to the south. The water’s distinctive color is caused by the presence of rock flour, a fine-grained silt formed by glacial ice grinding against rock.
This pair of satellite images illustrates how much both glaciers changed over a 26-year period and how that change affected the lake between them. The Thematic Mapper on Landsat 5 captured the top image on August 22, 1987. The Operational Land Imager aboard Landsat 8 acquired the bottom image on August 13, 2013. Turn on the comparison tool to slide between the two images.
Notice how much the terminus of each glacier has shifted. Novatak retreated by about 1 kilometer (0.6 miles); East Novatak moved back by about two. Also note how part of the lake changed color. As the terminus of East Novatak retreated up into a mountain valley, it cut off a small tributary that supplied meltwater to the western lobe of the lake. With the supply of rock flour cut off, that part of the lake became dark blue. Meanwhile, the other side expanded and changed shape as East Novatak retreated.
Most of East Novatak is below 1,000 meters (3,000 feet) in elevation, relatively low for an alpine glacier. “The retreat of this glacier, like that of nearby Yakutat, indicates how susceptible the Alaskan glaciers with lower-elevation accumulation zones are to our warming climate,” noted Mauri Pelto, a glaciologist and professor at Nichols College in his blog, From A Glaciers Perspective.
References and Related Reading
- Arendt, A. et al (2011) Assessing the Status of Alaska’s Glaciers. Journal of Glaciology, 59 (213), 149-161.
- Blackwelder, E. et al (1907) Glacial Features of the Alaskan Coast between Yakutat Bay and the Alsek River. Journal of Glaciology, 15 (5).
- Berthier, E. et al (2010, January 17) Contribution of Alaskan glaciers to sea-level rise derived from satellite imagery. Nature Geoscience, (3) 92-95.
- Molina, B.F. (2008) Glaciers of Alaska: Satellite Image atlas of glaciers of the world. U.S Geological Survey Professional Paper, 1386-K, 525.
- Pelto, M. (2009, December 5) Yakutat Glacier Rapid Retreat, Alaska. Accessed August 7, 2014.
- Pelto, M. (2014, January 12) East Novatak Glacier Retreat, Alaska. Accessed August 7, 2014.
- Trüssel, B. et al. (2013) Rapid thinning of lake calving Yakutat Glacier and the collapse of the Yakutat Icefield, Southeast Alaska. Journal of Glaciology, 59 (213), 149-161.
NASA Earth Observatory image by Robert Simmon, using Landsat data from the U.S. Geological Survey. Caption by Adam Voiland.
This image record originally appeared on the Earth Observatory. Click here to view the full, original record.