Swiss glaciers 1850–2100

Gornergletscher

Gorner Glacier

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 41.23km² Area in 2016 · ±0% compared with 2016

The second-largest glacier in Switzerland, below Monte Rosa near Zermatt. Where it meets the Grenzgletscher, an ice-dammed lake, the Gornersee, fills most summers and drains through the glacier within days. A dam at its foot is among the 15 hydropower projects agreed in 2021.

Area 201641.23km²2nd largest
Elevation2,190–4,599mmedian 3,364 m
Length13.4kmfaces north-west
1850 ice body65.5km²now 4 glaciers
Tongue since 1882−3,094m124 measurements
Thinning 1931–2023−53maverage surface lowering
Ice left in 210022%of 2020 volume, SSP2-4.5

Gornergletscher is the 2nd-largest glacier in Switzerland, covering 41.23 km² in the canton of Valais. Its ice spans 2,190 to 4,599 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 65.5 km², which has since split into 4 glaciers covering 54.1 km² in 2016 (−17%). Its tongue has been measured 124 times since 1882. In total it has retreated 3,094 m, about 21.8 m a year. Between 1931 and 2023 its surface dropped by 53 m on average. With strong climate protection (SSP1-2.6), about 43% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5), 2% would remain. Its meltwater is projected to peak around 2037.

Pictures

Then and now

ThenAround 1890–1900, with Monte Rosa and the Lyskamm. Photochrom print, Library of Congress.
Around 1890–1900, with Monte Rosa and the Lyskamm. Photochrom print, Library of Congress. Photochrom Print Collection · Public domain · Wikimedia Commons
NowGornergletscher in 2006.
Gornergletscher in 2006. No machine-readable author provided. Mathein assumed (based on copyright claims) · CC BY 2.5 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions43%52% left in 2050
SSP2-4.5 · intermediate emissions22%53% left in 2050
SSP3-7.0 · high emissions8%50% left in 2050
SSP5-8.5 · very high emissions2%42% left in 2050
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210043%22%8%2%
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

05010015020025020102030205020702090
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 1882

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

−4,000 m−3,000 m−2,000 m−1,000 m0 m1,000 m190019251950197520002025−3,094 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1931

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

−60 m−40 m−20 m0 m19401960198020002020−53 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

185065.55 km²193162.44 km²197359.52 km²201641.23 km²2050 · SSP2-4.532.81 km²2100 · SSP2-4.518.53 km²

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

SGI id
B56-07
Canton
Valais
River
Rhône → Mediterranean
Basin
Vispa
Location
45.9407° N, 7.8256° E · swisstopo map
Elevation
2,190–4,599 m, median 3,364 m
Slope, aspect
19°, north-west
Debris cover
3.13 km² (8% of the area)
Inventory image
2015
Ice volume (model)
≈ 5.01 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02822, RGI60-11.02875, RGI60-11.02894, RGI60-11.02903, RGI60-11.02912, RGI60-11.02919 …
In 1850 joined with
Monte Rosagletscher, Breithorngletscher (Zermatt), Unterer Theodulgletscher
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/
  5. Huss et al. (2007). Glacier-dammed lake outburst events of Gornersee, Switzerland. Journal of Glaciology 53. www.cambridge.org/core/journals/journal-of-glaciology/article/glacierdammed-lake-outburst-events-of-gornersee-switzerland/556C5B9A155B3FE3D5CAA2A3FDDE64B3
  6. Gemeinsame Erklärung des Runden Tisches Wasserkraft (2021). www.newsd.admin.ch/newsd/message/attachments/69601.pdf

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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