Swiss glaciers 1850–2100

Glacier de Cheilon

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 3.51km² Area in 2016 · ±0% compared with 2016
Area 20163.51km²57th largest
Elevation2,684–3,641mmedian 2,972 m
Length3.6kmfaces north
Area since 1850−42%6.00 km² in 1850
Tongue since 1924−1,267m93 measurements
Thinning 1988–2023−33maverage surface lowering
Ice left in 21000%of 2020 volume, SSP2-4.5

Glacier de Cheilon is the 57th-largest glacier in Switzerland, covering 3.51 km² in the canton of Valais. Its ice spans 2,684 to 3,641 m and faces north. Its meltwater drains to the Rhône and on to the Mediterranean. In 1850, at the end of the Little Ice Age, it covered 6.00 km²; by 2016 it had lost 42% of that area. Its tongue has been measured 93 times since 1924. In total it has retreated 1,267 m, about 12.7 m a year. Between 1988 and 2023 its surface dropped by 33 m on average. With strong climate protection (SSP1-2.6), about 6% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2069. Its meltwater is projected to peak around 2031.

Pictures

In pictures

Glacier de Cheilon in 2007.
Glacier de Cheilon in 2007. 4000er · Public domain · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions6%12% left in 2050
SSP2-4.5 · intermediate emissionsGoneIce gone around 2091
SSP3-7.0 · high emissionsGoneIce gone around 2081
SSP5-8.5 · very high emissionsGoneIce gone around 2069
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%202020402060208021006%0%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

0510152020102030205020702090
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 1924

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

−1,500 m−1,250 m−1,000 m−750 m−500 m−250 m0 m19401960198020002020−1,267 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1988

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

−40 m−30 m−20 m−10 m0 m1990200020102020−33 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18506.00 km²19314.96 km²19734.56 km²20163.51 km²2050 · SSP2-4.50.92 km²2100 · SSP2-4.50.06 km²

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

SGI id
B74-08
Canton
Valais
River
Rhône → Mediterranean
Basin
Hérens & Nendaz
Location
46.0080° N, 7.4220° E · swisstopo map
Elevation
2,684–3,641 m, median 2,972 m
Slope, aspect
19°, north
Debris cover
1.30 km² (37% of the area)
Inventory image
2016
Ice volume (model)
≈ 0.195 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02749
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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