The snowiest ski resort in Europe.
What makes Warth-Schröcken a place where snow is an integral part of winter?
The answer does not lie on the ski slopes, but at a small snow-measuring station at Körbersee. For decades, observations, measurements and records have been kept here to determine exactly how much snow actually falls from the sky.
From exceptional snowfall to the unique location in the Arlberg region and modern snowmaking: the story of ‘Europe’s snowiest ski resort’ begins with a close look at nature.
From exceptional snowfall to the unique location in the Arlberg region and modern snowmaking: the story of ‘Europe’s snowiest ski resort’ begins with a close look at nature.
A snow festival steeped in tradition.
Ulrike Schlierenzauer’s working day begins early in the morning. At the snow station on Lake Körbersee, she measures the amount of fresh snow that has fallen, monitors the wind and weather, and records the characteristics of the snowpack.
These measurements are far more than just local weather observations. The data is incorporated into the daily avalanche report for the state of Vorarlberg and also forms the basis for long-term snow statistics.
A look back shows just how extraordinary the snowfall in Warth-Schröcken can be: in the winter of 1998/99, a total of 16.50 metres of fresh snow was recorded between November and the end of April. Even in one of the winters with the least snow that the Schlierenzauer family can remember, the total still amounted to around 5.50 metres.
Figures like these explain why snow in Warth-Schröcken is not merely a winter phenomenon, but shapes the character of the region.
These measurements are far more than just local weather observations. The data is incorporated into the daily avalanche report for the state of Vorarlberg and also forms the basis for long-term snow statistics.
A look back shows just how extraordinary the snowfall in Warth-Schröcken can be: in the winter of 1998/99, a total of 16.50 metres of fresh snow was recorded between November and the end of April. Even in one of the winters with the least snow that the Schlierenzauer family can remember, the total still amounted to around 5.50 metres.
Figures like these explain why snow in Warth-Schröcken is not merely a winter phenomenon, but shapes the character of the region.
How Warth-Schröcken set a snowfall record.
The fact that Warth-Schröcken became known as a region with particularly heavy snowfall is due in no small part to an English ski journalist. Fraser Wilkin conducted extensive research into snowfall patterns and weather conditions in the Alpine region and compared long-term measurement data from various ski resorts.
In 2008, he published his findings in the British daily newspaper Daily Mail. For Warth-Schröcken, he calculated a long-term average snowfall of around 10.70 metres per year. This placed the region at the top of his comparison.
Since this publication, Warth-Schröcken has been described as Europe’s snowiest ski resort. The key factor here is the consideration of annual snowfall – that is, the total amount of fresh snow that has fallen over the course of a winter, rather than the depth of the snow cover on any given day.
The title therefore has a measurable basis: it is based on snowfall data recorded over the long term and the region’s specific geographical and meteorological conditions.
When the north brings snow.
But why does it snow so much here in particular?
A key factor is the so-called northern barrier effect. Moist air masses frequently move across the Alpine region from the north to the north-west. When they encounter the mountains around the Arlberg, these air masses are forced to rise. As this happens, the air cools, moisture condenses – and snow can form.
Warth-Schröcken is situated in a particularly favourable position. The region lies at around 1,500 metres above sea level and is surrounded by mountains that cause the moist air masses from the north to rise.
Added to this are numerous north- and east-facing slopes. These receive comparatively little direct sunlight in winter and are able to retain their natural snow cover for a long time.
The result is a combination that winter sports enthusiasts particularly appreciate: plenty of natural snowfall, a long-lasting snow cover and often good conditions well into spring.
A key factor is the so-called northern barrier effect. Moist air masses frequently move across the Alpine region from the north to the north-west. When they encounter the mountains around the Arlberg, these air masses are forced to rise. As this happens, the air cools, moisture condenses – and snow can form.
Warth-Schröcken is situated in a particularly favourable position. The region lies at around 1,500 metres above sea level and is surrounded by mountains that cause the moist air masses from the north to rise.
Added to this are numerous north- and east-facing slopes. These receive comparatively little direct sunlight in winter and are able to retain their natural snow cover for a long time.
The result is a combination that winter sports enthusiasts particularly appreciate: plenty of natural snowfall, a long-lasting snow cover and often good conditions well into spring.
Snow is part of everyday life here.
For the locals, the extraordinary amount of snow has long been part of everyday life. Whilst visitors delight in the fresh powder snow, a lot of snow initially means extra work: roads and paths have to be cleared, roofs checked and vehicles dug out.
Nevertheless, for the Schlierenzauer family, snow is an integral part of life at Körbersee. Long-term measurements repeatedly show just how varied a winter can be.
Another striking fact is: The heaviest snowfalls in Warth-Schröcken often don’t occur until later in the winter. Considerable amounts can still fall, particularly in March and April.
This explains why the region isn’t just worth visiting at the start of the season. It’s also worth taking a look at the slopes in spring.
Nevertheless, for the Schlierenzauer family, snow is an integral part of life at Körbersee. Long-term measurements repeatedly show just how varied a winter can be.
Another striking fact is: The heaviest snowfalls in Warth-Schröcken often don’t occur until later in the winter. Considerable amounts can still fall, particularly in March and April.
This explains why the region isn’t just worth visiting at the start of the season. It’s also worth taking a look at the slopes in spring.
When nature gets a helping hand.
However much snow there may be in Warth-Schröcken, natural snow cannot be planned for. Modern snow-making systems are therefore used to ensure a reliable start to the season and consistent conditions on the slopes.
In Warth-Schröcken, water from the Panoramasee is used for this purpose. Together with compressed air, it is finely atomised in so-called nucleator nozzles. This creates tiny crystal nuclei to which further water droplets can attach. As they fall to the ground, these form snow crystals.
The quality depends on many factors – including temperature, humidity, water and the correct settings on the snow-making equipment. Although the system is computer-controlled, staff also monitor the slopes and snow conditions directly on site.
Making snow is therefore not simply a matter of switching on a machine. Experience, knowledge of the weather and precise coordination are crucial to ensuring that the snow is deposited where it is needed.
In Warth-Schröcken, water from the Panoramasee is used for this purpose. Together with compressed air, it is finely atomised in so-called nucleator nozzles. This creates tiny crystal nuclei to which further water droplets can attach. As they fall to the ground, these form snow crystals.
The quality depends on many factors – including temperature, humidity, water and the correct settings on the snow-making equipment. Although the system is computer-controlled, staff also monitor the slopes and snow conditions directly on site.
Making snow is therefore not simply a matter of switching on a machine. Experience, knowledge of the weather and precise coordination are crucial to ensuring that the snow is deposited where it is needed.
Natural snow and artificial snow complement each other.
Warth-Schröcken’s unique character therefore stems from the interplay of several factors: its location at around 1,500 metres above sea level, the frequent north-facing wind-sheltered conditions, the orientation of many of the slopes, and the exceptional natural snowfall.
The modern snow-making system complements these natural conditions and provides additional planning certainty – particularly at the start of the winter season or when certain weather patterns bring less precipitation.
Anyone driving through Warth-Schröcken or skiing on the slopes therefore sees only part of the story. Behind the wintry landscape lie decades of measurements, meteorological peculiarities and people who work every day to ensure that the natural conditions are transformed into the best possible conditions for winter sports.
And perhaps that is precisely what makes the ‘snowiest ski resort in Europe’ so special: here, snow is not just a figure in a statistic. It shapes the landscape, everyday life and the winter sports experience in equal measure.
The modern snow-making system complements these natural conditions and provides additional planning certainty – particularly at the start of the winter season or when certain weather patterns bring less precipitation.
Anyone driving through Warth-Schröcken or skiing on the slopes therefore sees only part of the story. Behind the wintry landscape lie decades of measurements, meteorological peculiarities and people who work every day to ensure that the natural conditions are transformed into the best possible conditions for winter sports.
And perhaps that is precisely what makes the ‘snowiest ski resort in Europe’ so special: here, snow is not just a figure in a statistic. It shapes the landscape, everyday life and the winter sports experience in equal measure.