Easter holidays full of change / Delicate avalanche situation in some southern regions

Spring is already palpable, in all its facets: deep winter at high altitudes in southern regions. Fresh snow and storm-strength winds have generated (and still do) far-reaching often trigger-prone snowdrift masses. At lower altitudes the snowpack is becoming quite moist/wet and this will continue over the next few days. We expect numerous loose-snow avalanches in extremely steep terrain, and also increasingly frequent glide-snow avalanches on steep grass-covered slopes, even on north-facing slopes depending on the degree of wetness. Danger pattern cold-on-warm may have formed a near-surface weak layer locally/regionally since 23 March. Currently, this is relevant on shady slopes above 2200 m in southern regions.

Capricious weather

Last week was marked by highly fluctuating weather: W/NW airstreams and southern barrier clouds. At high altitudes, a strong to stormy wind was frequently blowing.

Aprilwetter Ende März: Auflockerungen, Niederschlag, Wind, ein Auf und Ab bei den Temperaturen...
April weather at the end of March: bright spells, precipitation, winds, fluctuating temperatures…
Das Föhndiagramm zeigt eindrucksvoll den großen Luftdruckunterschied zwischen Bozen und Innsbruck. Je größer die Luftdruckdifferenz desto stärker weht der Föhn. Rot: Südföhn / Blau: Nordföhn
The foehn diagram depicts graphically the huge disparities in air pressure between Bolzano and Innsbruck. The bigger the difference, the stronger the foehn blows. Red: southerly foehn / blue: northerly foehn

The marked cold front on 23.03 with storm-strength gusts, plummeting temperatures and thunderstorm-like precipitation was striking.

Eine Kaltfront brachte anfangs Niederschläge vermehrt im Westen des Landes... (72h Neuschneesumme zwischen 22.03. und 24.03.)
A cold front brought precipitation initially to the western regions… (72-hr map of overall fresh snow on 22-24.03)
Am 23.03. und 24.03. fiel Schnee bis in tiefe Lagen (Foto: 24.03.2024 © LWD Tirol)
On 23 and 24 March there was snowfall down to low lying areas. (photo: 24.03.2024 © LWD Tirol)
Vom 27.03. auf den 28.03. Neuschnee v.a. in den südlichen Regionen
Fresh snow on 27-28.03, esp. in southern regions

Snowdrift accumulations: assess with caution at high altitudes

Main problem currently (28.03.2024): fresh and recently generated snowdrift accumulations. Weak layer for the snowdrifts repeatedly observed last week: increasing, often massive layers of graupel, deposited in several bouts during the showerlike precipitation since the middle of last week.

Graupel als ernst zu nehmende Schwachschicht. Außerfern (Foto: 25.03.2024 © Stefan Zangerl)
Graupel, a serious weak layer. Ausserfern (photo: 25.03.2024 © Stefan Zangerl)
Snow plumes on the mountaintops: a sign of far-reaching snow transport. (photo: 25.03.2024 © Anton Riepler)

Two surprisingly large-surface avalanche releases were reported from the Arlberg region. One was due to explosives, one a release presumably because a cornice broke. The primary fracture was generated when a layer of graupel was articifially triggered, a secondary fracture occurred when a more deeply embedded faceted layer atop a melt-freeze crust was struck. At the time of the avalanches the slab was particularly well established for a brief time following stormy conditions.

Lawinenabgänge Schindlergrat: Auslösung durch Sprengungen (Foto: 25.03.2024 © Simon Guem)
Avalanche releases on Schindlergrat: artificially triggered by explosives (photo: 25.03.2024 © Simon Guem)
Avalanche release Gamskarspitze in Arlberg region (photo: 25.03.2024 © Markus Lorenz)

As a rule, reported avalanches were small-sized, a few were medium, always near ridgelines or behind discontinuities in the terrain and usually on shady slopes. The blanketed fresh snow was a short-term weak layer.

Slab near ridgeline in Höllensteinkar, Zillertal Alps (photo: 25.03.2024 © Markus Stadler)
Ridgeline slide in Ausserfern (photo: 25.03.2024 © Marvin Kärle)
Ridgeline slab, Zillertal Alps (photo: 23.03.2024 © Alexander Radlherr)

Possible “cold on warm” weak layer

We are groping our way in the dark, but it seems that on shady slopes around 2200m since 23.03 locally or regionally a weak layer has formed due to danger pattern cold-on-warm. A report today (28.03) from southern Zillertal corroborates this suspicion. The prerequisites exist since temperatures plummeted on Saturday, 23.03: a moist snowpack surface blanketed by cold fresh snowfall. In principle, this phenomenon is also relevant (up to 2600m?) for the southern regions which have recently received fresh snowfall. We would be grateful for any and all reports from outlying terrain (please include altitude!), mailed to lawine@tirol.gv.at

Dieses Schneebrett auf 2250m Nord in den südlichen Zillertaler Alpen dürfte auf einer kantigen Schicht oberhalb einer Schmelzharschkruste abgegangen zu sein. (Foto: 28.03.2024 © Stefan Wierer)
This slab at 2250m North in southern Zillertal Alps was probably due to a faceted layer atop a melt-freeze crust. (photo: 28.03.2024 © Stefan Wierer)
Die Voraussetzungen für gm.4 (kalt auf warm) waren gegeben, dort wo der Neuschnee vom 23.03. auf einer feuchten Schneeoberfläche zu liegen gekommen ist. Blau: Bildungszeitraum einer möglichen Schwachschicht,
The prerequisites for gm.4 (cold-on-warm) existed wherever fresh snowfall on 23.03 was deposited on a moist snowpack surface. Blue: formation period of a possible weak layer.

Gliding snow: latent danger

Last week the snowpack was thoroughly moist until 23.03 due to rain impact. This had an effect on gliding snow activity (which later tapered off). However, we do not get tired of telling you: circumvent zones below glide cracks.

Die gelben Kreise zeigen in Summe 6 Personen in einem Klettersteig im Nahbereich der Franz-Senn-Hütte. Darüber befindet sich ein Hang mit Rissen und Aufwölbungen in der Schneedecke (Foto: 19.03.2024 © Horst Fankhauser)
The yellow circles depict 6 persons on a prepared climbing route near the Franz-Senn-Hütte. Above them is a wall with shooting cracks and convexities in the snowpack. (photo: 19.03.2024 © Horst Fankhauser)
Yellow circle shows the area of the climbing route which was swept over by a huge glide-snow avalanche on 23.03.2024. (photo: © Thomas Fankhauser)

What’s next?

Warmth penetrating the snowpack, diffuse solar radiation, these will make the snowpack moister. We expect increasingly frequent moist/wet loose-snow avalanches in extremely steep terrain starting on 29.03.2024. Glide-snow avalanches can also be heightened in equal measure.

At high altitudes, fresh and recently generated snowdrift accumulations are the big problem. Stormy winds are again coming to the mountains. From Sunday to Monday in the southern regions, significant amounts of fresh snow are expected. In the southern Ötztal Alps, about 50cm of fresh snow is anticipated. Thus, the situation for winter sports enthusiasts remains delicate in the southern regions at high altitudes where snowfall will be heavy.

Visibility will be poor at times, making it difficult to evaluate the dangers on-site. In order to reduce the risk, particularly in southern regions, lots of experience and much self-restraint are called for.

Further north, conditions will be better. Nevertheless, in springtime tiny weather changes bring big changes in avalanche danger over very short periods. For that reason, ongoing information and acute observation of backcountry terrain and quick reacting to the conditions are of paramount importance.

The entire team of the Avalanche Warning Service of Tirol wishes all of you Happy Easter! (As soon as the avalanche situation changes and we have information about it, we will publish another blog.)