Reichert Glacier Rapid Retreat, Northern Patagonia Icefield, Chile

Reichert Glacier (Reicher) is at the northwest corner of the North Patagonia Icefield (NPI) and flows west from the Mont Saint Valentin region and ends in the expanding Reicher Lake. Rivera et al (2007) notes that the glacier was named for French geologist Federico Reichert, but that Reicher has ended up as the established spelling. They further note that the glacier lost 4.2 square kilometers of area from 1979 to 2001 and had an ELA of 1330 m. The glacier has two main icefalls, one at the first bend in the glacier above the terminus at 400 m, the second at the ELA from 1100-1600 m. Davies and Glasser (2012) identify the most rapid area loss of -0.77% per year to the 1986-2001 period. The glacier retreated rapidly from 1987-1997, but the terminus was stabilized from 1997-2001, before retreating again to near the 2014 terminus by 2002.
reicher glacier ge 2013
2013 Google Earth image
Here we examine Landsat imagery from 1986, 1997 and 2014 to document the changes. The pink arrow indicates the 1987, terminus, the yellow arrow the 1998 terminus and the red arrow the 2014 terminus. In 1987 the glacier terminates close to the southern end of Reicher Lake, pink arrow. By 1998 the glacier has retreated to the yellow arrow and is terminating on the west side of Reicher Lake across the lake from the main glacier valley. By 2014 the glacier has retreated into the main glacier valley and Reicher Lake extends 8.8 km from the northeast to southwest. A new lake has developed in 2014 above the first icefall, orange arrow. This lake indicates a potential second lake basin beginning to develop in the glacier reach above the first icefall. If this is the case another rapid retreat will ensue, though not in the immediate future. The glacier retreated 6.7 km from 1987 to 2014, with 90% of the retreat occuring by 2002. Area extent loss is 8-9 square kilometers. The lower icefall is 1.5 km from the current terminus, and indicates the maximum extent of Reicher lake and the retreat that can be enhanced by calving into that lake. This glacier has followed the pattern of the neighboring Gualas Glacier just to its south. WHOI-Oceanus recently published an interesting article on this glacier. The retreat is emblematic of the entire NPI as noted by both Rivera et al (2007) and Davies and Glasser (2012) work, the latter had an excellent Figure 8 indicating two periods of fastest recession since 1870, are 1975-1986 and 2001-2011 for NPI glaciers. This retreat includes that of Steffen Glacier, Nef Glacier, and Colonia Glacier.

reicher  glacier 1897
1987 Landsat image

reicher glacier 1998
1998 Landsat image

reicher glacier 2014
2014 Landsat image

Glaciar Gualas Retreat lake expansion, Patagonia, Chile

Glaciar Gualas drains from the northwest portion of the Northern Patagonia Icefield (NPI) into a rapidly expanding new lake Laguna Gualas. There is a spectacular icefall (I) where the glacier descends from the main NPI from 1600 m to 900 m, which is below the equilibrium line. Below this point the Gualas has a 2 km wide, 15 km long valley reach extending to the terminus which currently has a substantial calving face into Laguna Gualas (A-B). Point M inidcates an area of substantial moraine cover on the ice, that will with continued retreat be a likely location for a new lake to form, much as the periodic lake at Point C. Lopez and Cassasa (2011) have documented a 1.8 km retreat from 2001-2011 of this glacier, updating and expanding on the work of Rivera et al (2007). This is part of the ongoing inventory of Chilean glacier and the NPI, that is being undetaken by the Laboratory of Glaciology at the Centre for Engineering Innovation CECS (CIN), Valdivia, Chile. This project has built on initial joint work with Glacier and Cryospheric Environment Research Laboratory in Japan and now with NASA-JPL as well. The Japan Aerospace Exploration Agency with Glacier and Cryospheric Environment Research Laboratory published a comparison of selected NPI glacier retreats. Here we compare Landsat satellite images of the glacier from 1987, 2001, 2005 and 2011 illustrating the retreat that Lopez and Casassa (2011) have chronicled. They have further noted an average thinning of the valley tongue of 2.1 meters per year from 1975-2005 and a doubling in the rate of area lost, 2.8 square kilometers, from 2001-2011 versus 1975-2001. In 1987 the glacier essentially fills the lake basin, margin is indicated with pink dots. By 2001 an evident fringe of water separates the glacier from the lake margin on all but the eastern side of the lake. In 2005 the margin is hard to discern given the extensive floating icebergs in the lake. By 2011 the lake is evident and the glacier has retreated 2.2 km from its 1987 position. There is little additional change from 2011 to 2014. This retreat is like those of other NPI glaciers such as, Reichert Glacier, Steffen Glacier, Nef Glacier, and Colonia Glacier.
1987 Landsat image

2001 Landsat image

2005 Landsat image
gualas glacier 2014
2014 Landsat image

The glacier surface is steep in the first kilometer behind the terminus, indicating a rising bedrock under the glacier. Then the glacier has a very modest slope for the next 14 km. As long as the glacier can calve into a lake, this will enhance retreat. The current lake may not end at the bedrock step just behind the current terminus. However, even if this occurs the low slope above that point indicates another basin that will have sufficient depth to form a second lake basin. It is unlikely that the calving retreat of this glacier will have more than a temporary interruption. In the annotated Google Earth view below the approximate elevations along the glacier are listed. What is of particular interest is the 2.1 meter per year thinning on the lower glacier has occurred while on the upper glacier there is a small amount thickening (Rivera et al;, 2007). This implies the retreat is driven by enhanced melting due to warming, since the only way to thicken the glacier in the accumulation zone is via increased snowfall.