More than 5% of Switzerland’s glacial ice vanished in 2026, say scientists

More than 5% of Switzerland’s glacial ice vanished in 2026, say scientists

A winter with little snow followed by an exceptionally warm summer has led to a year of rapid melting in the European country.

L. Hoesli


New data has revealed that more than 5 per cent of Switzerland’s glacial ice disappeared in 2026, with some of the country’s smaller glaciers vanishing entirely. 

On average, glacier thickness decreased by 2.5m–4m, and some glaciers lost up to 10m of ice from their tongues (a strip of ice that sticks out from the bottom of a glacier). 

The Rhône, Clariden and Aletsch glaciers experienced their greatest melts on record. Meanwhile, Bella Tola in Valais and Griessfirn in Glarus disappeared completely.

Glaciers are melting faster than ever before in Switzerland. Credit: ETH Zürich

Why are Switzerland's glaciers melting?

Experts from the Swiss Academy of Sciences (SCNAT) say the excessive melt rates were the result of a mild winter with relatively little snowfall, followed by extremely hot and dry conditions between May and September 2026, when around 2.2 trillion litres of water were released from the country’s glaciers.

By the end of summer, any snow that had fallen on the glaciers over winter was gone, leaving them exposed to the heat of the sun.

This year’s ice loss follows a sustained period of high melt rates. In the past five years, nearly 20 per cent of Switzerland’s glacier volume has gone.

The researchers say the new data, reported by GLAMOS – Glacier Monitoring Network’s long-term monitoring of Swiss glaciers – highlights how rapidly the country’s glacial landscape is changing. 

In pictures: Switzerland’s glaciers

Rhone Glacier
In many places, deep collapse pits can be seen on glacier tongues, as shown here on the Rhône Glacier. Huge cavities beneath the ice suddenly collapse – a phenomenon that further accelerates the retreat. Credit: M. Huss
Morteratsch
The glacier terminus of the Vadret da Morteratsch. Credit: L. Hösli
Findel Glacier
Glaciologists on the Findel Glacier. The ice around the Matterhorn continues to recede dramatically, and the glacier’s foreland, with its lakes and scree, is expanding. Credit: M. Huss

Aletsch
Water flowing through blue caves beneath the Great Aletsch Glacier. Credit: M. Huss
Piz Palu
Piz Palü is typical of the landscape of the Swiss high mountains in the summer of 2026: grey mountains and glaciers with numerous crevasses. Credit: M. Huss
Rhone
Once the ice has receded, the first plants soon begin to colonise the area, bringing life to the scree-covered wasteland. Credit: M. Huss
Rhone Glacier
The tongue of the Rhône Glacier with an impressive glacier gate. Credit: M. Huss
Vadret dal Murtèl
Re-drilling a measuring rod on the Vadret dal Murtèl. Credit: M. Huss
Findel Glacier
Meltwater from the Findel Glacier is collected for electricity generation. Forty years ago, the glacier still stood right next to the water intake. Credit: M. Huss
Clariden Glacier
The Claridenfirn is completely free of snow in September 2026. Credit: M. Huss

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Top image: Aletsch Glacier, Switzerland. Credit: L. Hoesli

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