Swiss glaciers 1850–2100

Glacier de Boveire

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 1.66km² Area in 2016 · ±0% compared with 2016
Area 20161.66km²103rd largest
Elevation2,685–3,634mmedian 3,245 m
Length2.5kmfaces north-west
Area since 1850−31%2.42 km² in 1850
Tongue since 1889−259m62 measurements
Thinning 1983–2024−25maverage surface lowering
Ice left in 21000%of 2020 volume, SSP2-4.5

Glacier de Boveire is one of 1,400 glaciers in Switzerland, covering 1.66 km² in the canton of Valais. Its ice spans 2,685 to 3,634 m and faces north-west. Its meltwater drains to the Rhône and on to the Mediterranean. In 1850, at the end of the Little Ice Age, it covered 2.42 km²; by 2016 it had lost 31% of that area. Its tongue has been measured 62 times since 1889. In total it has retreated 259 m, about 1.9 m a year. Between 1983 and 2024 its surface dropped by 25 m on average. With strong climate protection (SSP1-2.6), about 1% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2055. Its meltwater peaked around 2023.

Future

What remains in 2100

SSP1-2.6 · low emissions1%Ice gone around 2084
SSP2-4.5 · intermediate emissionsGoneIce gone around 2065
SSP3-7.0 · high emissionsGoneIce gone around 2063
SSP5-8.5 · very high emissionsGoneIce gone around 2055
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%202020402060208021001%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

02.55.07.520102030205020702090
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 1889

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

−300 m−200 m−100 m0 m100 m200 m300 m1900192019401960198020002020−259 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1983

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

−30 m−20 m−10 m0 m1990200020102020−25 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18502.42 km²19312.16 km²19732.07 km²20161.66 km²2050 · SSP2-4.50.85 km²2100 · SSP2-4.50.00 km²

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

SGI id
B84-04
Canton
Valais
River
Rhône → Mediterranean
Basin
Dranse
Location
45.9660° N, 7.2610° E · swisstopo map
Elevation
2,685–3,634 m, median 3,245 m
Slope, aspect
22°, north-west
Debris cover
0.19 km² (11% of the area)
Inventory image
2016
Ice volume (model)
≈ 0.055 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02814
Nearby

More in the Dranse basin

All glaciers in this basin →

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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