Swiss glaciers 1850–2100

Vadret da Porchabella W

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 1.43km² Area in 2016 · ±0% compared with 2016
Area 20161.43km²118th largest
Elevation2,695–3,266mmedian 2,876 m
Length2.0kmfaces north
1850 ice body3.8km²now 2 glaciers
Tongue since 1893−1,528m115 measurements
Thinning 1991–2022−29maverage surface lowering
Ice left in 21000%of 2020 volume, SSP2-4.5

Vadret da Porchabella W is one of 1,400 glaciers in Switzerland, covering 1.43 km² in the canton of Graubünden. Its ice spans 2,695 to 3,266 m and faces north. Its meltwater drains to the Rhine and on to the North Sea. In 1850 it was part of a larger ice body of 3.8 km², which has since split into 2 glaciers covering 1.5 km² in 2016 (−60%). Its tongue has been measured 115 times since 1893. In total it has retreated 1,528 m, about 11.7 m a year. Between 1991 and 2022 its surface dropped by 29 m on average. With strong climate protection (SSP1-2.6), about 1% of its 2020 ice would remain in 2100. With very high emissions (SSP5-8.5) it would be gone around 2053. Its meltwater is projected to peak around 2026.

Pictures

In pictures

Vadret da Porchabella W in 2004.
Vadret da Porchabella W in 2004. Luidger at German Wikipedia · CC BY-SA 3.0 · Wikimedia Commons
Future

What remains in 2100

SSP1-2.6 · low emissions1%Ice gone around 2074
SSP2-4.5 · intermediate emissionsGoneIce gone around 2064
SSP3-7.0 · high emissionsGoneIce gone around 2062
SSP5-8.5 · very high emissionsGoneIce gone around 2053
SSP1-2.6SSP2-4.5SSP3-7.0SSP5-8.5
0%25%50%75%100%202020402060208021001%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

02.04.06.08.020102030205020702090
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 1893

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

−2,000 m−1,500 m−1,000 m−500 m0 m500 m1900192019401960198020002020−1,528 m
GLAMOS Swiss Glacier Length Change, release 2025.

Thinning since 1991

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

−30 m−20 m−10 m0 m199520002005201020152020−29 m
GLAMOS Swiss Glacier Volume Change, release 2025.
Profile

Facts

Area over time

18503.80 km²19312.91 km²19732.35 km²20161.43 km²2050 · SSP2-4.50.23 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
A12e-04
Canton
Graubünden
River
Rhine → North Sea
Basin
Alpine Rhine
Location
46.6270° N, 9.8822° E · swisstopo map
Elevation
2,695–3,266 m, median 2,876 m
Slope, aspect
18°, north
Debris cover
0.39 km² (27% of the area)
Inventory image
2015
Ice volume (model)
≈ 0.052 km³ in 2020 (OGGM)
RGI ids
RGI60-11.01267
In 1850 joined with
Vadret da Porchabella NW
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: SteilimigletscherSmaller: Glärnischfirn →