These are not groundbreaking new findings, but the cross-national message once again clarifies what we basically already know: Higher temperatures mean rising snowfall limits, means less snow, especially at low altitudes. It generally snows less (it rains instead) and snow that has fallen melts again more quickly. Phases with continuous snow cover at low altitudes start later and end earlier. The number of days with snow cover in Vienna, Innsbruck and Graz has decreased by around 30% in the last 90 years or so. The figures are similar on the Swiss Plateau. In Munich, too, there are on average around 20 fewer days with snow today than in the 1950s. While the temperature determines the amount of snow at low altitudes, the amount of precipitation is decisive at high altitudes. Although it is also getting warmer in the high mountains, it is usually still cold enough for snow instead of rain.
The weather services emphasize that the temperature and, above all, winter precipitation fluctuate greatly from year to year and that long-term trends are not always easy to identify, as they are overlaid by regionally different, short-term effects. Despite long-term warming, cooler winters can occur in the meantime. Similarly, there can also be a lot of snow at low altitudes - it just doesn't happen as often.
If emissions remain high, it can be assumed that snow cover in Austria will decrease by 90% at low altitudes by 2100, and by 50% at around 1500m. In Switzerland, it is estimated that snow cover below 1000m will decrease by 80% by 2060, and by 30 to 50% above 1500m. But we don't have to give up because everything is lost anyway: climate protection measures can still counteract this development. If the goals of the Paris Climate Agreement are achieved, the expected decrease in snow cover would be roughly halved, according to the weather services.