Swiss glaciers 1850–2100

Langgletscher

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 8.01km² Area in 2016 · ±0% compared with 2016
Area 20168.01km²25th largest
Elevation2,103–3,894mmedian 3,005 m
Length4.8kmfaces south
1850 ice body12.5km²now 3 glaciers
Tongue since 1888−920m118 measurements
Thinning 1927–2023−32maverage surface lowering
Ice left in 210014%of 2020 volume, SSP2-4.5

Langgletscher is the 25th-largest glacier in Switzerland, covering 8.01 km² in the canton of Valais. Its ice spans 2,103 to 3,894 m and faces south. Its meltwater drains to the Rhône and on to the Mediterranean. In 1850 it was part of a larger ice body of 12.5 km², which has since split into 3 glaciers covering 8.4 km² in 2016 (−33%). Its tongue has been measured 118 times since 1888. In total it has retreated 920 m, about 6.8 m a year. Between 1927 and 2023 its surface dropped by 32 m on average. With strong climate protection (SSP1-2.6), about 29% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5), 4% would remain. Its meltwater peaked around 2018.

Pictures

In pictures

Langgletscher in 2005.
Langgletscher in 2005. Roland Zumbühl (Picswiss), Arlesheim (Commons:Picswiss project) · CC BY-SA 3.0 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions29%53% left in 2050
SSP2-4.5 · intermediate emissions14%52% left in 2050
SSP3-7.0 · high emissions7%52% left in 2050
SSP5-8.5 · very high emissions4%41% left in 2050
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%2020204020602080210029%14%7%4%
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 1888

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

−1,000 m−750 m−500 m−250 m0 m250 m1900192019401960198020002020−920 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1927

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

185012.51 km²193110.48 km²19739.52 km²20168.01 km²2050 · SSP2-4.54.74 km²2100 · SSP2-4.51.45 km²

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

SGI id
B31-04
Canton
Valais
River
Rhône → Mediterranean
Basin
Lötschental–Aletsch
Location
46.4673° N, 7.9496° E · swisstopo map
Elevation
2,103–3,894 m, median 3,005 m
Slope, aspect
21°, south
Debris cover
0.87 km² (11% of the area)
Inventory image
2017
Ice volume (model)
≈ 0.449 km³ in 2020 (OGGM)
RGI ids
RGI60-11.01698, RGI60-11.01728, RGI60-11.01799, RGI60-11.01835
In 1850 joined with
Jegigletscher E, Schinhorn W
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.

← Larger: Oberer GrindelwaldgletscherSmaller: Obers Ischmeer E →