Shrinking glaciers
The melting of Switzerland’s glaciers has been observed for many years. Since the end of the Little Ice Age around 1850, the volume of glaciers in Switzerland has decreased by more than half. As temperatures increase, glaciers melt faster and precipitation falls more often as rain than as snow. When glaciers melt, the important “glacial reservoir” of the water balance changes.
At the moment, glaciers are not in equilibrium with the current climate conditions. Were the climate to remain as it is today, the glaciers would continue to shrink over the next several decades to half of their current volume. However, experts expect an increase in temperature of 3°C by the year 2085 (plus or minus one degree). This warming will have severe repercussions for Swiss glaciers: according to models, only 20 to 30% of the current glacier volume will remain by 2100. Most of the remaining glacier volume will be in the Rhone catchment area, thanks to the largest glacier in Switzerland, the Aletsch.

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ForumAlpinum 2026
With a focus on environmental challenges, socio-economic transformations and adaptation strategies, the ForumAlpinum 2026 positions itself as a moment of multidisciplinary technical-scientific and political reflection on the consequences of deglaciation in Alpine regions (and beyond), with particular attention to environmental, cultural and economic impacts.
Image: Andrea Omizzolo
And Swiss glaciers continue to melt
Glacial melting in Switzerland was once again enormous in 2025. A winter with low snow depth combined with heat waves in June and August led to a loss of three per cent of the glacier volume. This is the fourth largest level of shrinkage since measurements began. Consequently, the ice mass reduced by one quarter in the last ten years. This was reported by GLAMOS, the glacier monitoring network in Switzerland, and the Swiss Commission for Cryosphere observation (SCC) of the Swiss Academy of Sciences.
Image: Matthias HussSchweizer Kryosphärenbericht 2023/2024
Trotz viel Schnee: Weiterer Rückgang von Gletscher und Permafrost in den Schweizer Alpen
Image: SKK
