In den Skigebieten werden die letzten Wintervorbereitungen getroffen, wie hier am Bild in der Schlick die Wartung der Sprenganlagen. (© Dominik Jenewein, 29.10.2025)

Review of first onset of winter this season

As was forecast, it snowed as much as 50cm in the western regions, locally even more, on Monday, 27.10. For a brief spell, you even had to watch out for slab, glide-snow and loose-snow avalanches. The higher temperatures which followed in its wake provided a swift decrease in avalanche danger and rapid melting of the snowpack, on sun-exposed sites in particular.

Isolated avalanche prone locations for slab avalanches are currently to be found on very steep, glaciated slopes in high alpine regions.

Weather, snow, avalanches

The weather

An analysis of the precipitation depicts the distribution of overall precipitated amounts on 27.10.2025. The focal point lay in the far west, followed by the northern and eastern regions of North Tirol,.

Niederschlagsanalyse vom 27.10.2025: Am meisten Niederschlag fiel im Westen des Landes © Wetterbox
Precipitation analysis from 27.10.2025: most of the precipitation fell in the far western regions.
Ein Blick auf die Wetterstation am Stubaier Gletscher: Die vergangene Woche war eher unbeständig mit Neuschnee und teilweise stürmischem Wind.Temperaturanstieg.
A glance at the Stubai Glacier weather station: last week was relatively unfavorable due to fresh fallen snow plus storm-strength winds from region to region, including a marked rise in temperature.

The snowpack

Taking into consideration avalanche releases in the glaciated regions at high altitude, what most interests us is a lengthy view in the rear-view mirror of what happened weather-wise. There have been bouts of fresh snowfall since September after which some snow remained on the ground in certain regions, or spots, at least in shady, high alpine, glaciated terrain.

Die Wetterstationsgrafik am Pitztaler Gletscher zeigt den Wetterverlauf seit Anfang September. Niederschläge fielen teilweise als Schnee, schmolzen meist wieder dahin, blieben aber in größerer Höhe zum Teil auch liegen.
The graph at the Pitztal Glacier weather station depicts the course of weather since the beginning of September. Precipitation often fell as snow, then melted, except in some places at great heights.

The upshot from the cocktail of snowfall plus dry, warm periods was, as can be seen in the image of the snow profile on the Stubai Glacier depicted below, a “crust sandwich” consisting of faceted snow crystals and melt-freeze crusts at its base.

Das Schneeprofil am Daunferner in den Stubaier Alpen zeigt oberhalb der Gletscheroberfläche eine Abfolge von kantigen Kristallen und Krusten. Kantige Kristalle dienten im Nahbereich des Profilortes als Schwachschicht für Schneebrettlawinen, welche am 28.10. von WintersportlerInnen ausgelöst wurden. (© Günter Chwojan, 29.10.2025)
In this snow profile from the Daunferner glacier in the Stubai Alps, we find above the immediate surface of the glacier a sequence of faceted crystals and crusts. Faceted crystals serve as a weak layer for slab avalanches in the nearby vicinity of the spot where the profile was taken, which were triggered by winter sports enthusiasts on 28 October. The “slab” (measuring from 30cm to 85cm) was generated by snowfall including wind impact starting on 27.10.2025. (© Günter Chwojan, 29.10.2025)

The fresh snow was transported by the strong-to-storm strength winds. At heightened altitudes, wide-ranging transported snow masses were deposited.

Der Neuschnee wurde umfangreich verfrachtet. Grieskogelgruppe. (© LWD Tirol, 28.10.2025)
Snow transport in the Grieskogel Massif. (© LWD Tirol, 28.10.2025)

In the meantime, measurable amounts of the fresh snow have melted, including in the regions where snowfall was heavy…

Blick vom Galzig am Arlberg Richtung Osten (© foto-webcam.eu, 28.10.2025)
View from Galzig am Arlberg looking eastwards, one day after the snowfall. (© foto-webcam.eu, 28.10.2025)

Blick vom Galzig am Arlberg Richtung Osten vier Tage nach den Schneefällen. Die Schneedecke beginnt zunehmend auzuapern. (© foto-webcam.eu, 28.10.2025)
View from Galzig am Arlberg looking eastwards four days after the snowfall. The snowpack is already beginning to melt itself bare. (© foto-webcam.eu, 28.10.2025)

Some rainfall on 30.10 up to about 2500m led to a moistening of the snowpack surface, even on shady slopes.

Die Kurven zeigen die "trockene" Schneefallgrenze, also jenen Höhenbereich, ab dem Schnee trocken fällt für die Westliche Verwallgruppe. Der letzte Niederschlag am 30.10. fiel ab etwa 2500m aufwärts trocken.
The undulating curve depicts the “dry” snowfall level, in other words, the altitude as of which the snowfall is dry, in the western Verwall massif. The final precipiation on 30.10 fell as dry snow only starting at about 2500m.
Gebietsweiser Niederschlag am 30.10. Meist waren es wenige mm mit Schwerpunkt in den südlichen Ötztaler Alpen (um 10mm).
Depiction of precipitation region-by-region on 30.10. Most of it was only a few millimetres, with the focal point in the southern Ötztal Alps (about 10mm).

The avalanches

As mentioned, avalanche activity was observed just as anticipated: most of the releases unleashed in the form of small glide-snow avalanches across steep grass-covered slopes.

Kleine Gleitschneelawinen am Vorderen und Hinteren Sonnenkogel im Außerfern (© Thomas Lutz, 31.10.2025)
Glide-snow avalanche on Vordere and Hintere Sonnenkogel in Ausserfern (© Thomas Lutz, 31.10.2025)

On the Stubai Glacier, several winter sports enthusiasts triggered medium-magnitude slab avalanches in the near-ground level weak layers atop the glacier ice on Tuesday, 28.10.2025. According to our information, no injuries were suffered.

Von WintersportlerInnen ausgelöste Schneebrettlawinen am Daunferner in den Stubaier Alpen (© Günter Chwojan, 28.10.2025)
Slab avalanches triggered by winter sports enthusiasts on Daunferner glacier in the Stubai Alps (© Günter Chwojan, 28.10.2025)
Spontane Schneebrettlawine unterhalb der Weißkugel in einem extrem steilen O-Hang (während oder kurz nach den Schneefällen vom 27.10.2025) (© foto-webcam.eu, 29.10.2025)
Naturally triggered slab avalanche below the Weisskugel on an extremely steep east-facing slope (either during or shortly after the snowfall of 27.10.2025) (© foto-webcam.eu, 29.10.2025)

Outlook

Above-average temperatures for this juncture of the season, accompanied by strong-velocity southerly foehn wind. Thus, we are ushered into the weekend.

Der Patscherkofel als Gradmesser für den Südföhn.
Patcherkofel as litmus paper for the southerly foehn wind.

On Sunday, 02.11, according to Geosphere Austria (GSA), the “foehn wind will collapse due to a cold front from the west. In the morning in Ausserfern, rainfall will set in, subsequently the rain will expand its scope into the Lower Inn Valley and East Tirol. The rainfall will often be heavy, and strong-velocity gust-laden westerly winds will be blowing. Large-scale amounts of precipitation are possible, particularly in the regions near the Main Alpine Ridge and in East Tirol. The snowfall level is expected to descend to 1500 metres by Sunday evening. Prior to the cold front, it will be mild (10 to 15 degrees), thereafter temperatures will drop measurably.” Following this little scenario there will be lots of sunshine and temperatures will again rise as the coming week gets underway.

24h Neuschneeprognose für Sonntag (Allerseelen), den 02.11.2025. Der Niederschlagsschwerpunkt liegt am östlichen Alpenhauptkamm.
24-hr forecast for Sunday, 02.11.2025 (All Souls Day). The focal point of precipitation will lie in the eastern sector of the Main Alpine Ridge.

During and following the snowfall: watch out for slab avalanches for a brief spell!

A situation similar to the one on 27.10 is being generated in the regions where snowfall is heaviest. At heightened altitudes there will be strong-velocity, gusty westerly winds which generate freshly formed snowdrift masses. Thus: Avoid fresh snowdrifts in very steep terrain at high altitudes and in high alpine regions. At high altitudes, the proneness to triggering of these drifts will rapidly decrease following the end of the precipitation.

A special degree of caution is called for in high alpine regions, to be specific, in glaciated, very steep terrain. In those places, the near-ground weak layers consisting of faceted crystals referred to above could well be triggerable by winter sports enthusiasts, and thereby unleash slab avalanches.

The next blog will be published whenever the avalanche situation deteriorates seriously.