Swiss glaciers 1850–2100

Turtmanngletscher 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 10.71km² Area in 2016 · ±0% compared with 2016
Area 201610.71km²18th largest
Elevation2,306–4,150mmedian 3,245 m
Length5.5kmfaces north-west
1850 ice body15.1km²now 6 glaciers
Tongue since 1885−3,027m124 measurements
Thinning 1931–2023−32maverage surface lowering
Ice left in 21007%of 2020 volume, SSP2-4.5

Turtmanngletscher zentral is the 18th-largest glacier in Switzerland, covering 10.71 km² in the canton of Valais. Its ice spans 2,306 to 4,150 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 15.1 km², which has since split into 6 glaciers covering 11.4 km² in 2016 (−25%). Its tongue has been measured 124 times since 1885. In total it has retreated 3,027 m, about 21.9 m a year. Between 1931 and 2023 its surface dropped by 32 m on average. With strong climate protection (SSP1-2.6), about 22% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2081. Its meltwater peaked around 2023.

Pictures

In pictures

Turtmanngletscher zentral in 2005.
Turtmanngletscher zentral in 2005. Steinmann · Public domain · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions22%51% left in 2050
SSP2-4.5 · intermediate emissions7%48% left in 2050
SSP3-7.0 · high emissions1%Ice gone around 2099
SSP5-8.5 · very high emissionsGoneIce gone around 2081
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210022%7%1%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

0102030405020102030205020702090
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 1885

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 m1900192019401960198020002020−3,027 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.

−40 m−30 m−20 m−10 m0 m19401960198020002020−32 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

185015.14 km²193113.98 km²197312.74 km²201610.71 km²2050 · SSP2-4.57.88 km²2100 · SSP2-4.51.76 km²

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

SGI id
B60-09
Canton
Valais
River
Rhône → Mediterranean
Basin
Anniviers & Turtmann
Location
46.1200° N, 7.7020° E · swisstopo map
Elevation
2,306–4,150 m, median 3,245 m
Slope, aspect
18°, north-west
Debris cover
0.89 km² (8% of the area)
Inventory image
2016
Ice volume (model)
≈ 0.661 km³ in 2020 (OGGM)
RGI ids
RGI60-11.02490, RGI60-11.02507, RGI60-11.02522
In 1850 joined with
Chanzilti, Stierbärg, Unnamed glacier B60-24, Turtmanngletscher S 1, Turtmanngletscher S2
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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