After long-awaited snowfall in January, parts of the Alps are now covered with fresh powder and happy skiers. But the Swiss side of the iconic mountain range had the driest December since record-keeping began over 150 years ago, and 2016 was the third year in a row with scarce snow over the Christmas period. A study published today in The Cryosphere, a journal of the European Geosciences Union, shows bare Alpine slopes could be a much more common sight in the future.

The new research, by scientists based at the Institute for Snow and Avalanche Research (SLF) and at the CRYOS Laboratory at the École Polytechnique Fédérale in Switzerland, shows that the Alps could lose as much as 70% of snow cover by the end of the century. However, if humans manage to keep global warming below 2°C, the snow-cover reduction would be limited to 30% by 2100.

In addition to the changes in snow cover, the new research reveals the Alpine winter season – the period when natural snow is deep enough for winter sports – is set to become shorter. The team say that, as temperatures rise, the ski season could start half a month to a month later than it does at present. Moreover, if we don’t cut emissions, enough snow for winter sports can only be guaranteed above 2500 m by the end of the century.

“The Alpine snow cover will recede anyway, but our future emissions control by how much,” explains lead-author Christoph Marty, a research scientist at SLF.

Higher greenhouse gas emissions will bring higher temperatures to the Alps. But scientists were less sure about how global warming would affect snowfall in the region. “The majority of the climate models used project slightly increasing winter precipitation towards the end of the century. However, since temperatures are clearly increasing simultaneously we may experience increasing rainfall and not snow fall,” Marty explains. “We hope our results convincingly show that even increasing winter precipitation cannot compensate for the effect of the strongly increasing temperatures.”

By simulating future snow cover in the Alps for various temperature and snowfall projections, the team was able to make more robust projections of how Alpine snow will change in the future, and how sensitive this change will be to different global-warming scenarios. Co-author Sebastian Schlögl, also from SLF, explains: “We used meteorological data and many different climate change scenarios to model the future snow cover in two Alpine catchments with ALPINE3D.” ALPINE3D is an open-source computer model designed to simulate how snow is distributed in mountainous regions.

The team’s projections show that the layer of snow covering the Alps will get less deep “for all elevations, time periods and emission scenarios,” they write in their The Cryosphere paper. “The most affected elevation zone for climate change is located below 1200 m, where the simulations show almost no continuous snow cover towards the end of the century.” About a quarter of the ski resorts in the Alps are located fully below this altitude, according to the skiresort.info website.

Ski resorts at higher altitude could also see drastic reductions in snow depth. If global warming isn’t limited to 2°C, snow depth could decrease by about 40% at the end of the century even for elevations above 3000 m. The Zugspitze, the highest mountain in Germany, has an altitude of 2962 m. The two highest ski resorts in the Alps, the French Aiguille du Midi in Chamonix, Mount Blanc and the Swiss-Italian Matterhorn ski paradise, have maximum elevations of about 3900 m and minimum heights of around 1000 m and 1500 m, respectively.

The decreasing snow depth and a shorter snow season will impact tourism in the Alps. “Since many Alpine villages are heavily dependent on winter tourism, the economy and society of regions with such tourism centres will suffer,” says Schlögl. In the long term, the increased rainfall in winter, the smaller snow cover and disappearing Alpine glaciers will alter how much water flows into Alpine creeks and rivers and how the water volume changes over time. “This will not only impact the ecology, but also the management of water for irrigation, power production or shipping,” he adds.

Despite these impacts, the new research highlights how much we could save in the Alps by mitigating climate change. “The fact that we lose 30% of the Alpine snow cover with the 2°C global warming scenario is sad, but at the same time encouraging compared to the 70% loss when we go on with business as usual,” concludes Marty.

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Please mention the name of the publication (The Cryosphere) if reporting on this story and, if reporting online, include a link to the paper (http://www.the-cryosphere.net/11/517/2017/) or to the journal website (http://www.the-cryosphere.net).

This research is presented in the paper ‘How much can we save? Impact of different emission scenarios on future snow cover in the Alps’, published in the EGU open access journal The Cryosphere on 16 February 2017.

Citation: Marty, C., Schlögl, S., Bavay, M., and Michael, L.: How much can we save? Impact of different emission scenarios on future snow cover in the Alps, The Cryosphere, 11, 517–529, doi:10.5194/tc-11-517-2017, 2017

The team is composed of Christoph Marty (WSL Institute for Snow and Avalanche Research [SLF], Davos Switzerland), Sebastian Schlögl (SLF and Laboratory of Cryospheric Sciences [CRYOS], EPFL, Lausanne Switzerland), Mathias Bavay (SLF), Michael Lehning (SLF and CRYOS).

The European Geosciences Union (EGU) is Europe’s premier geosciences union, dedicated to the pursuit of excellence in the Earth, planetary, and space sciences for the benefit of humanity, worldwide. It is a non-profit interdisciplinary learned association of scientists founded in 2002 with headquarters in Munich, Germany. The EGU has a current portfolio of 17 diverse scientific journals, which use an innovative open access format, and organises a number of topical meetings, and education and outreach activities. Its annual General Assembly is the largest and most prominent European geosciences event, attracting over 13,000 scientists from all over the world. The meeting’s sessions cover a wide range of topics, including volcanology, planetary exploration, the Earth’s internal structure and atmosphere, climate, energy, and resources. The EGU 2017 General Assembly is taking place in Vienna, Austria, from 23 to 28 April 2017. For information about meeting and press registration, please check http://media.egu.eu, or follow the EGU on Twitter and Facebook.

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The Cryosphere (TC) is an international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of frozen water and ground on Earth and on other planetary bodies. The main subject areas are ice sheets and glaciers, planetary ice bodies, permafrost, river and lake ice, seasonal snow cover, sea ice, remote sensing, numerical modelling, in situ and laboratory studies of the above and including studies of the interaction of the cryosphere with the rest of the climate system.

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