Wind and lots of snow: considerable avalanche danger regionally

Heavy precipitation in far-reaching parts of North Tirol accompanied by often storm-strength NW winds have negatively affected avalanche danger levels. The snowdrift problem remains preeminent, avalanche prone locations have become far more frequent. In some places avalanches can be easily triggered and become highly dangerous for winter sports enthusiasts. We recommend a defensive route selection on the weekend. In addition, the activity of glide-snow avalanches has increased as a result of the recent loading atop the snowpack and rain impact.

The avalanche situation in central and southern East Tirol is more favorable. In these regions there is little change since last week.

Current situation

Snowdrift problem & potential persistent weak layer

The fresh snow and drifts from the last few hours have been deposited atop a favorable old snowpack at least up to 2200 m, which is significantly moistened due to the marked rise in temperatures and rainfall on 24 January. The warmth dissolved all the weak layers near the snowpack surface. Fresh snow and drifts below 2200 m are bonding well with the moistened snowpack surface.

At higher altitudes the situation is different: possible short-lived weak layers inside the fresh snow and snowdrifts in the form of loose fresh snow. With ascending altitude such avalanche prone locations become more frequent.

Potential (long-lived) weak layers may have been generated near a melt-freeze crust which formed as of 9 January in the form of faceted crystals. We assume a potential danger particularly on sunny slopes (E/S/W) above 2400 m, on shady slopes potential between 2200 and 2400 m. This applies particularly to regions where snowfall has been heavy. We look forward to reports from observers on-site (snobs.live).

An especially beautiful snapshot of faceted crystals beneath a melt-freeze crust. The variable weather conditions last week led to melt-freeze crusts forming on which faceted crystals then developed. These constitute potential weak layers for slab avalanches. (photo: 21.01.2024, ©Stefan Zangerl).
Persistent, i.e. long-enduring weak layer in the form of faceted crystals and cup-formed crystals atop a melt-freeze crust on a very steep west-facing slope at 2450 m in the Glockner Massif (link to profile).

As regards the coming sunny weekend we advise self-restraint in outlying terrain following this highly variable phase of weather conditions. Pay close heed to the fact that we have had a largely stable snowpack in recent weeks, and only small near-surface avalanches could be triggered. This situation has now changed. Danger zones are much more frequent and triggerings can have far greater consequences. In addition, there is uncertainty about how trigger-prone the weak layers beneath the fresh snow and drifts actually are. Our recommendation: to begin with, avoid the big, steep slopes and wait until the coming warmth gradually improves the situation.

Gliding snow problem & loose-snow avalanches

The precipitation has generated a load atop the snowpack which is reinforcing gliding snow activity. At intermediate altitudes the rainfall made the snowpack thoroughly wet. Over the next few days at intermediate altitudes (and also where snowfall was heavy), isolated large-sized glide-snow avalanches can be expected. This type of avalanche is always naturally triggered, and is thus utterly unpredictable. Pay close heed to the dangerous spots on your planned route and to potential runout zones, and insist on circumventing them whenever possible.

The gliding snow problem will persist. Fresh glide-snow avalanches in Mattun near St. Anton in the Lechtal Alps. (photo: 19.01.2024, ©Chris Riepl).

In addition, as a result of solar radiation and ongong mild temperatures on Friday, 26 January, numerous naturally triggered loose-snow avalanches can be expected in extremely steep terrain. Their magnitude will vary, depending on the amounts of fresh snow. The avalanche prone locations occur particularly on sunny, rocky slopes.

A short review

The last few days were marked by highly fluctuating temperatures. Rain, snow, wind, in all their variations, a roller-coaster of conditions for snow lovers. Initially some snowfall with little wind as temperatures plummeted (19 January), then beautiful winter days with temperatures rising continually. Then a succession of fronts emerging from a mild/moist and turbulent NW airstream. A cold front in the early hours of Thursday, 25 January, brought lots of precipitation regionally. The snowfall level on that evening was above the timberline to start with, descended incrementally during the night down to intermediate altitudes.

Last week at Hochgasser weather station in the Venediger Massif. Last Saturday, 20 January, measured a bitter cold -20°C, then temperatures rose over days that followed. What affected the snowpack most of all was the warm front on Tuesday night (23.1) and the moist-warm weather that immediately followed. With the cold front on Thursday, temperatures dropped again somewhat. The fresh snowfall was often accompanied by stormy winds.
Precipitation on Friday, 19.01.2024, was with little wind in some regions. The snowpack base was often hard and dry loose-snow avalanches were able to reach long runouts. (photo: 20.01.2024, ©Gabriel Falkner).
Feather snow: characterized by extremely low density due to the snow crystals falling amid little wind and very low temperatures, permitting them to be deposited without any deformation. Crystals resemble goose down feathers that capture lots of air in their complex filigree structure, making the snow particularly light. (photo: 19.01.2024, ©Elisabeth Zangerl).
A small naturally triggered slab avalanche behind a discontinuitiy in the terrain, Granatspitz range in East Tirol. This photo is a good example of the small, near-surface snowdrift accumulations which were the big avalanche problem until the middle of last week. On the other side of the trench, a glide crack. The quite narrow trench in the deposit zone is a striking discontinuity in the terrain where even a small avalanche can lead to a critical burial beneath snow masses. (photo: 20.01.2024, ©Toni Riepler).
Surface hoar, often observed last week, was destroyed by wind and warmth. In photo, lightly blanketed surface hoar on Gleinser Mähdern at 1600 m. (photo: 21.01.2024, ©Dominik Jenewein).
Due to higher temperatures and rain impact on Wednesday, 24.01, there were numerous naturally triggered wet-snow and glide-snow avalanches. (photo: 24.01.2024, ©Adi Kerber).
Near-surface slab avalanches on Stubai Glacier. They triggered due to the impulse of higher temperatures from the warm front including higher rainfall level up to over 2600 m on Tuesday night (23.01). (photo: 24.01.2024, ©Günter Chwojan).
The cold front during the night and early morning hours of 24 January brought lots of precipitation regionally. The focal point lay from the Allgäu Alps to the eastern Karwendel where more than 60mm was registered in places. (©Hydro Online).
Even as the precipitation tapered off winds remained strong, transporting the fresh snow far-reachingly, as here in the Hohe Tauern. (photo: 25.01.2024, ©LWD Tirol).

Outlook

What’s next? First a brief quiet period until Friday afternoon, 26 January, followed by a weak cold front, bringing some precipitation on Friday night. Winds will again be strong and will transport the fresh snow. On the weekend, tranquil conditions will follow and persist for awhile. A period of mild beautiful weather will follow.

Forecast for fresh snow, 26.01.
Black line: forecast of the middle wind which will significantly slacken off starting on Saturday, 27 January.
Temperature trend in the next few days. The zero-degree level will ascend to nearly 3000 m. Much too mild for the end of January. (©Oberlandwetter).
Fresh snowfall? Unlikely until at least the end of next week.