High avalanche danger regionally – naturally triggered avalanches expected

Up to 150 cm of fresh fallen snow and storm-strength winds are creating a critical avalanche situation regionally, with High avalanche danger (level 4). Increasingly frequent naturally triggered releases are expected during the period of intensive precipitation, with numerous avalanche prone locations for winter sports enthusiasts. In the major areas of precipitation the dangers in outlying terrain are extreme.

Swiftly rising avalanche danger

GeoSphere forecasts are clear as day: intensive snowfall and rainfall in many parts of the land over the next few days. On top of that, storm-strength, sometimes gale-strength winds. Snowfall level around 1200 m, with deviations due to wind and intensity of precipitation. Currently (21.12.2023 at 6:00 pm) precipitation has begun in the western regions. Rainfall level at the moment: 1500-1800 m.

Deteriorating weather conditions, rising temperatures, stormy winds, starting snowfall in western Lechtal Alps

48-hour fresh snow forecast 21.12.2023 at 1:00 am until 23.12.2023 at 1:00 am: major areas of precipitation west of Wipptal and Hohe Tauern. (c) Geosphere Austria

It will be unusually stormy. (forecast for 22.12.2023 2:00 pm) (c) Geosphere Austria

Forecast of precipitation, wind and snowfall level for western Verwall Range region. Striking: not merely the intensity but the rapid increase of wind impact. (c) Geosphere Austria
Avalanche danger will increase swiftly to high above the timberline from region to region on 22.12.2023. In southern East Tirol conditions are most favourable.

Avalanche problems

High danger above the timberline due to marked snowdrift problem in all aspects, large expected avalanches and the start of very poor snowpack stability. When a snowdrift problem prevails, danger zones can be recognized pending good visibility.

Below the timberline in the areas of major snowfall, the dominant problem is the fresh fallen snow, with possible weak layers inside it. Danger zones here cannot be recognized.

In addition, a marked gliding snow problem persists below 2400 m, in fact is getting worse.

Snowpack analysis: basis of avalanche scenarios

As often mentioned in recent blogs, snow depths are above average for this juncture of the season. Quite often the snowpack is very compact. Weak layers inside the old snowpack are, thus, not widespread. In principle this is a good pre-requisite for the intensive precipitation we anticipate. Our focus is directed at the snowpack surface and the potential weak layers there:

In zones which have been wind-protected until now, esp. on north-facing slopes, the snowpack surface is still loose ragged crystals or slightly faceted forms of crystals.

The arrow points to loose powder as potential weak layer for the snow deposited on top of it. The powder will be worked on by the wind and transported. So one will find such a surface only in wind-protected terrain, on leeward slopes and similar areas.

On steep sunny slopes a thin melt-freeze crust has formed over the last few days due to the high temperatures and solar radiation. At altitudes above 2400 m up to 2800 m, expansively metamorphosed crystals formed just below this crust.

Snow profile to exemplify a potential weak layer. Here is a profile at 1650 m with a crust on the surface and a soft layer beneath it. Above 2400 m, faceted and ragged crystals were found beneath the crust which formed during the nights of clear skies. This occurred mainly on west and east-facing slopes.

In the lower part of the snowpack there is a series of crusts and some soft layers. Snowpack analysis shows only isolated fractures and potential weak layers. We assume that a fracture in this area is most possible in the southwestern regions of North Tirol (Samnaun range, Kaunergrat, Glockturm range, Weisskugel range, Gurgler range).

In this profile in the Schlick (Kalkkögel) there was no fracture produced at the base. But the series of crusts and soft layers is visible.

Avalanche Weiss-See Joch towards Krummgampental; north, 2580 m. The avalanche triggered when winter sports enthusiasts were descending, fracturing in a weak layer near ground level. This is the only avalanches we know of triggering from a ground-level weak layer in outlying terrain which was much skied on during the recent period of beautiful weather – an indicator of isolated trigger sensitivity. (photo: Alpinpolizei, 17.12.2023).

Due to the high amount of rain in the snowpack, but also due to the early snow blanketing the ground, the snowpack is moist/wet at least up to intermediate altitudes. If the snowpack is compact, it can easily glide over steep smooth surfaces such as grassy slopes or smooth rock plates. The gliding snow activity will be heightened by the rain impact which is forecast, but also enhanced by the weight of the snow on top of it.

The arrow points to the snow:ground borderline. The snowpack there is 0°C.

Lots of gliding snow in the regions of Tirol where snowfall has been heaviest, such as here in the Northern Massif above Innsbruck (elipses). The arrows point to heightened loose-snow avalanches last weekend in sunny, extremely steep terrain. (photo: LWD Tirol, 18.12.2023)
One of the pre-requisites for a gliding snowpack over smooth steep surfaces is a moist/wet snowpack at the base, such as in this photo in the Schlick (Kalkkögel). (photo: LWD Tirol, 19.12.2023)

High avalanche risk in outlying terrain

Over the next few days, winter sports enthusiasts will be taking great risks in backcountry. For that reason, we advise keeping away from steep slopes and to be very mindful of avalanche runout zones.

Outlook

The critical avalanche situation will presumably last until Sunday, 24.12.2023. Thereafter we expect continuing improvements in the situation.