Swiss glaciers 1850–2100

Riedgletscher

IceIce lost since 1850This glacier

Past extents come from the Swiss Glacier Inventories of 1850, 1931, 1973 and 2016. Future extents are illustrative: each glacier’s projected area (OGGM, median of CMIP6 climate models) is removed from its lowest ice upward. About the scenarios.

Inventory 7.23km² Area in 2016 · ±0% compared with 2016
Area 20167.23km²28th largest
Elevation2,365–4,280mmedian 3,474 m
Length5.3kmfaces north-west
1850 ice body9.0km²now 2 glaciers
Tongue since 1895−1,591m67 measurements
Thinning 1930–2021−22maverage surface lowering
Ice left in 21006%of 2020 volume, SSP2-4.5

Riedgletscher is the 28th-largest glacier in Switzerland, covering 7.23 km² in the canton of Valais. Its ice spans 2,365 to 4,280 m and faces north-west. Its meltwater drains to the Rhône and on to the Mediterranean. In 1850 it was part of a larger ice body of 9.0 km², which has since split into 2 glaciers covering 7.3 km² in 2016 (−19%). Its tongue has been measured 67 times since 1895. In total it has retreated 1,591 m, about 12.4 m a year. Between 1930 and 2021 its surface dropped by 22 m on average. With strong climate protection (SSP1-2.6), about 36% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2080. Its meltwater peaked around 2020.

Pictures

In pictures

Riedgletscher.
Riedgletscher. ZachT · Public domain · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions36%65% left in 2050
SSP2-4.5 · intermediate emissions6%63% left in 2050
SSP3-7.0 · high emissions0%Ice gone around 2097
SSP5-8.5 · very high emissionsGoneIce gone around 2080
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210036%6%0%0%
Ice volume as a share of 2020, median of 14 climate models; shaded: middle two-thirds of models. OGGM v1.6.

Meltwater

Million m³ of water per year, 11-year mean

010203020102030205020702090
Water leaving the glacier area each year: ice melt, snowmelt and rain. It rises while the glacier melts faster, then falls as the ice runs out: “peak water”.
Measured

The record

Length change since 1895

Position of the glacier tongue, measured in the field almost every year. Hover for each measurement.

−2,000 m−1,500 m−1,000 m−500 m0 m500 m1900192019401960198020002020−1,591 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1930

Average change in surface height, from comparing elevation models made from maps, aerial images and laser scans.

−25 m−20 m−15 m−10 m−5 m0 m19401960198020002020−22 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18508.98 km²19318.52 km²19738.31 km²20167.23 km²2050 · SSP2-4.55.80 km²2100 · SSP2-4.51.39 km²

Past areas are the ice body this glacier belonged to at the time. Projections: OGGM median, SSP2-4.5.

SGI id
B54-03
Canton
Valais
River
Rhône → Mediterranean
Basin
Vispa
Location
46.1280° N, 7.8600° E · swisstopo map
Elevation
2,365–4,280 m, median 3,474 m
Slope, aspect
19°, north-west
Debris cover
0.44 km² (6% of the area)
Inventory image
2017
Ice volume (model)
≈ 0.497 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02495
In 1850 joined with
Riedgletscher
Sources

Sources

  1. Linsbauer et al. (2021). The new Swiss Glacier Inventory SGI2016. Frontiers in Earth Science 9. doi.org/10.3389/feart.2021.704189
  2. Mannerfelt et al. (2022). Halving of Swiss glacier volume since 1931 observed from terrestrial image photogrammetry. The Cryosphere 16. doi.org/10.5194/tc-16-3249-2022
  3. GLAMOS – Glacier Monitoring Switzerland. www.glamos.ch
  4. Zekollari et al. (2024). Twenty-first century global glacier evolution under CMIP6 scenarios and the role of glacier-specific observations. The Cryosphere 18 (OGGM v1.6 projections). tc.copernicus.org/articles/18/5045/2024/

Relief: swisstopo swissALTIRegio. 1850 and 1973 outlines: Maisch et al. (2000), Müller et al. (1976), Paul (2004). Length, mass balance and volume change: GLAMOS releases 2025. All sources and methods.

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