Swiss glaciers 1850–2100

Oberaargletscher

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 3.95km² Area in 2016 · ±0% compared with 2016
Area 20163.95km²51st largest
Elevation2,331–3,369mmedian 2,889 m
Length4.7kmfaces north-east
1850 ice body8.5km²now 2 glaciers
Tongue since 1858−2,035m88 measurements
Thinning 1927–2023−66maverage surface lowering
Ice left in 21000%of 2020 volume, SSP2-4.5

Oberaargletscher is the 51st-largest glacier in Switzerland, covering 3.95 km² in the canton of Bern. Its ice spans 2,331 to 3,369 m and faces north-east. Its meltwater drains to the Rhine and on to the North Sea. In 1850 it was part of a larger ice body of 8.5 km², which has since split into 2 glaciers covering 4.3 km² in 2016 (−49%). Its tongue has been measured 88 times since 1858. In total it has retreated 2,035 m, about 12.3 m a year. Its mass balance has been measured since 2014: on average −1.47 m of water equivalent per year, with the most negative year in 2022 (−2.83 m). Between 1927 and 2023 its surface dropped by 66 m on average. With strong climate protection (SSP1-2.6), about 7% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2062. Its meltwater peaked around 2014.

Pictures

In pictures

Oberaargletscher in 2006.
Oberaargletscher in 2006. --Cooper.ch 08:44, 27 August 2006 (UTC) · CC BY-SA 3.0 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions7%21% left in 2050
SSP2-4.5 · intermediate emissionsGoneIce gone around 2088
SSP3-7.0 · high emissionsGoneIce gone around 2076
SSP5-8.5 · very high emissionsGoneIce gone around 2062
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%202020402060208021007%0%0%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

010203020102030205020702090
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 1858

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

−2,500 m−2,000 m−1,500 m−1,000 m−500 m0 m1875190019251950197520002025−2,035 m
GLAMOS Swiss Glacier Length Change, release 2025.

Mass balance 2014–2025

Ice gained (blue) or lost (red) over the whole glacier each year, in metres of water equivalent. Measured with stakes drilled into the ice.

−3.0−2.0−1.00.01.0201520202025
GLAMOS Swiss Glacier Mass Balance, release 2025. Cumulative since 2014: −17.6 m water equivalent.

Thinning since 1927

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

−75 m−50 m−25 m0 m19401960198020002020−66 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18508.47 km²19316.29 km²19735.18 km²20163.95 km²2050 · SSP2-4.51.16 km²2100 · SSP2-4.50.01 km²

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

SGI id
A54g-03
Canton
Bern
River
Rhine → North Sea
Basin
Upper Aare
Location
46.5274° N, 8.1810° E · swisstopo map
Elevation
2,331–3,369 m, median 2,889 m
Slope, aspect
21°, north-east
Debris cover
0.60 km² (15% of the area)
Inventory image
2018
Ice volume (model)
≈ 0.107 km³ in 2020 (OGGM)
RGI ids
RGI60-11.01509
In 1850 joined with
Scheuchzerhorn SE
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: BisgletscherSmaller: Furgggletscher →