Swiss glaciers 1850–2100

Glacier du Mont Miné zentral

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 10.05km² Area in 2016 · ±0% compared with 2016
Area 201610.05km²19th largest
Elevation2,063–3,704mmedian 3,229 m
Length5.3kmfaces north
Area since 1850−21%12.67 km² in 1850
Tongue since 1956−886m56 measurements
Thinning 1933–2023−35maverage surface lowering
Ice left in 21002%of 2020 volume, SSP2-4.5

Glacier du Mont Miné zentral is the 19th-largest glacier in Switzerland, covering 10.05 km² in the canton of Valais. Its ice spans 2,063 to 3,704 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 12.67 km²; by 2016 it had lost 21% of that area. Its tongue has been measured 56 times since 1956. In total it has retreated 886 m, about 13.2 m a year. Between 1933 and 2023 its surface dropped by 35 m on average. With strong climate protection (SSP1-2.6), about 16% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2074. Its meltwater is projected to peak around 2039.

Pictures

In pictures

Glacier du Mont Miné zentral in 2008.
Glacier du Mont Miné zentral in 2008. The hiker · CC BY-SA 3.0 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions16%56% left in 2050
SSP2-4.5 · intermediate emissions2%50% left in 2050
SSP3-7.0 · high emissionsGoneIce gone around 2088
SSP5-8.5 · very high emissionsGoneIce gone around 2074
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210016%2%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

020406020102030205020702090
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 1956

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

−1,000 m−800 m−600 m−400 m−200 m0 m1960197019801990200020102020−886 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1933

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 m19401960198020002020−35 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

185012.67 km²193111.66 km²197311.09 km²201610.05 km²2050 · SSP2-4.58.51 km²2100 · SSP2-4.50.64 km²

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

SGI id
B72-15
Canton
Valais
River
Rhône → Mediterranean
Basin
Hérens & Nendaz
Location
45.9963° N, 7.5550° E · swisstopo map
Elevation
2,063–3,704 m, median 3,229 m
Slope, aspect
16°, north
Debris cover
0.43 km² (4% of the area)
Inventory image
2016
Ice volume (model)
≈ 0.726 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02709
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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