Yes, Europe gets snow, and in many regions it’s a defining feature of winter. But the continent spans from the Arctic Circle to the Mediterranean, so snowfall varies enormously. Northern Scandinavia and high mountain ranges see snow cover for over 200 days a year, while large parts of Britain, France, and Spain remain snow-free year-round. Where you are in Europe matters far more than the simple yes or no.
Where Snow Is Heaviest
The snowiest parts of Europe fall into two categories: the far north and the high mountains. Scandinavian mountain regions rack up around 160 snow-covered days per year. The Alps of Switzerland and Austria, the Pyrenees along the French-Spanish border, and the Carpathian Mountains stretching through Romania and neighboring countries see similar numbers. At the extremes, some high-altitude and Arctic areas spend more than 200 days under snow cover.
Elevation plays a major role within these ranges. In the Alps, stations on the northern side of the mountains hold roughly 30% more snow than southern stations at the same elevation up to about 1,750 meters. Above 2,250 meters, heavy snowpack is reliable regardless of which side of the range you’re on. The snow season in the Alps typically runs from November through May, with the deepest accumulation between December and February.
Northern and Eastern Europe
Scandinavia, Finland, and the Baltic states experience long, reliable winters. In Estonia, snow cover lasts up to 180 days in the northern part of the country. Coastal Lithuania and Latvia see fewer snow days, closer to 30, because the Baltic Sea moderates temperatures along the coast. Across the region, snow generally begins forming in November and doesn’t fully melt until April.
January and February bring permanent snow cover across most of the Baltics, Poland, and Ukraine, meaning the snow that falls stays on the ground rather than melting between storms. Average air temperatures sit well below freezing during these months. When temperatures rise in April, rapid snowmelt can trigger significant spring flooding. One consistent pattern across Eastern Europe: snow cover duration increases from west to east as the climate becomes more continental and less influenced by the Atlantic Ocean.
Central Europe and the Lowlands
In the lowlands of Central Europe, first snow typically arrives in late November. Switzerland’s central lowlands see their first measurable snowfall in the last third of November, while western and northwestern areas wait until early December. Southern Swiss lowlands often don’t see snow until around Christmas. The earliest recorded first-snow dates in the northern Alps go back to late October, but that’s unusual.
Cities like Vienna, Munich, Prague, and Zurich get regular winter snow, though it may not stick around as long as in the mountains or the far north. Germany’s northern plains receive less snow than the Bavarian Alps to the south, and the snow that does fall at lower elevations melts more quickly between storms.
Southern and Mediterranean Europe
Snow in Southern Europe is a different story. The Mediterranean coast only sees snowfall during extreme weather events. Athens, for instance, recorded just 61 snow events over a 43-year period from 1958 to 2001. More than half of those lasted only a single day, and snow falling for more than two consecutive days was considered exceptional. Since 1982, Athens hasn’t reliably seen snow every year.
That said, the mountains of Southern Europe are a different matter entirely. Greece’s mountainous interior gets regular snow from November through May. The same applies to the higher elevations of Spain, southern France, and Italy. Ski resorts in the Italian Dolomites and even parts of southern Switzerland operate through April. It’s specifically the low-lying coastal areas of the Mediterranean that rarely see a flake.
What Drives Europe’s Snow Patterns
A major factor behind Europe’s snow distribution is the North Atlantic Oscillation (NAO), a large-scale pressure pattern over the Atlantic Ocean. When the NAO is in its positive phase, storm tracks shift northward, delivering more moisture and precipitation to Northern Europe while keeping Southern Europe drier. When it swings negative, cold air and storms push further south, sometimes bringing rare snowfall to Mediterranean cities.
Latitude and elevation are the two biggest predictors. Higher means snowier, and further north means snowier. But proximity to the ocean also matters. Coastal Western Europe, warmed by Atlantic currents, sees far less snow than inland areas at the same latitude. London sits further north than much of Poland, yet Warsaw gets significantly more snow days.
Europe’s Ski Season
If you’re planning a ski trip, the snow season across Europe’s major resorts generally runs from early December through late April. A handful of glacier resorts open earlier: Sölden in Austria opens in early October, and Zell am See’s Kitzsteinhorn glacier starts in mid-October. High-altitude French resorts like Tignes, Val Thorens, and Val d’Isère typically open in late November and stay open into early May.
Most mid-elevation resorts follow a December-to-April pattern. Chamonix, Verbier, and St. Anton open in December and close between mid-April and early May. Lower resorts like Morzine and Les Gets have shorter windows, often late December through mid-April. Italian resorts such as Cervinia (which shares glacier terrain with Zermatt) open in late October, while Cortina d’Ampezzo runs from late November to early April.
Snow Cover Is Declining
Europe’s snow is shrinking. A comprehensive analysis of Alpine weather stations from 1971 to 2019 found that average seasonal snow depth dropped by about 8.4% per decade. Maximum snow depth declined by 5.6% per decade, and the number of days with snow on the ground fell at the same rate. These declines showed up at nearly every station below 2,000 meters in elevation. Above that line, no consistent trend appeared, meaning high-altitude snow has held relatively steady while lower elevations lose ground.
Climate projections suggest the NAO will shift toward a more positive state under high-emissions scenarios, which would funnel more winter precipitation toward Northern Europe and reduce it in the south. For ski resorts and lowland communities that depend on winter snow, this means the snowline is creeping upward. Resorts below about 1,500 meters are increasingly relying on artificial snowmaking to maintain reliable seasons, while the highest Alpine terrain remains, for now, largely unaffected.