Swiss glaciers 1850–2100

Oberer Theodulgletscher

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. This glacier has no model run of its own; its future follows the typical path of glaciers its size.

Inventory 2.42km² Area in 2016 · ±0% compared with 2016
Area 20162.42km²66th largest
Elevation2,898–3,430mmedian 3,108 m
Length2.6kmfaces north
Area since 1850−49%4.78 km² in 1850
Thinning 1982–2023−38maverage surface lowering

Oberer Theodulgletscher is the 66th-largest glacier in Switzerland, covering 2.42 km² in the canton of Valais. Its ice spans 2,898 to 3,430 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 4.78 km²; by 2016 it had lost 49% of that area. Between 1982 and 2023 its surface dropped by 38 m on average. No glacier model run exists for it; on the map it follows the typical path of glaciers its size.

Measured

The record

Thinning since 1982

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 m1990200020102020−38 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18504.78 km²19314.08 km²19733.38 km²20162.42 km²2050 · SSP2-4.50.76 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
B56-30
Canton
Valais
River
Rhône → Mediterranean
Basin
Vispa
Location
45.9580° N, 7.7070° E · swisstopo map
Elevation
2,898–3,430 m, median 3,108 m
Slope, aspect
13°, north
Debris cover
0.00 km² (0% of the area)
Inventory image
2016
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

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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