Swiss glaciers 1850–2100

Bisgletscher

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 4.18km² Area in 2016 · ±0% compared with 2016
Area 20164.18km²50th largest
Elevation2,354–4,490mmedian 3,459 m
Length3.6kmfaces east
Area since 1850−19%5.13 km² in 1850
Tongue since 1900−81m13 measurements
Thinning 1982–2024−12maverage surface lowering
Ice left in 210020%of 2020 volume, SSP2-4.5

Bisgletscher is the 50th-largest glacier in Switzerland, covering 4.18 km² in the canton of Valais. Its ice spans 2,354 to 4,490 m and faces east. Its meltwater drains to the Rhône and on to the Mediterranean. In 1850, at the end of the Little Ice Age, it covered 5.13 km²; by 2016 it had lost 19% of that area. Its tongue has been measured 13 times since 1900. In total it has retreated 81 m, about 0.7 m a year. Between 1982 and 2024 its surface dropped by 12 m on average. With strong climate protection (SSP1-2.6), about 48% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2099. Its meltwater peaked around 2020.

Pictures

In pictures

Bisgletscher in 2025.
Bisgletscher in 2025. Carsten Steger · CC BY-SA 4.0 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions48%71% left in 2050
SSP2-4.5 · intermediate emissions20%69% left in 2050
SSP3-7.0 · high emissions4%66% left in 2050
SSP5-8.5 · very high emissions1%Ice gone around 2099
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210048%20%4%1%
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

05101520102030205020702090
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 1900

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

−100 m−80 m−60 m−40 m−20 m0 m1900192019401960198020002020−81 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1982

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

−15 m−10 m−5 m0 m1990200020102020−12 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18505.13 km²19315.08 km²19734.81 km²20164.18 km²2050 · SSP2-4.53.33 km²2100 · SSP2-4.51.44 km²

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

SGI id
B58-08
Canton
Valais
River
Rhône → Mediterranean
Basin
Vispa
Location
46.1130° N, 7.7180° E · swisstopo map
Elevation
2,354–4,490 m, median 3,459 m
Slope, aspect
26°, east
Debris cover
0.05 km² (1% of the area)
Inventory image
2015
Ice volume (model)
≈ 0.211 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02558, RGI60-11.02587
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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