Avalanche.report

Monday 13 January 2025

Published 12 Jan 2025, 18:49:00


Danger level

2400m
Avalanche Problem
Wind slab
2400m


Circumvent fresh snowdrifts. Caution: persistent weak layer.

Snowdrift accumulations which are prone to triggering have been generated particularly in gullies, bowls and behind protruberances in the landscape due to fresh snow and strong to storm-velocity winds. Snowdrifts can be triggered by one single skier and are expected to remain trigger-sensitive. Danger zones occur esp. on shady slopes above 2400m. Whumpf noises and glide cracks when you step onto the snowpack are indicators of danger. Avalanches can grow to medium size. Magnitude and frequency of danger zones will tend to increase with ascending altitude.

Snowpack

dp.6: cold, loose snow and wind
dp.1: deep persistent weak layer

As a result of strong winds, trigger-sensitive snowdrift accumulations have been generated esp. in gullies, bowls and behind protruberances in the landscape. The older snowdrifts lie deposited atop soft layers particularly on NW/N/SE facing slopes above 2400m. The old snowpack is faceted, expansively metamorphosed, often weak. The snowpack is highly diverse even over small areas.

Tendency

Snowdrift accumulations to slowly stabilize over the next few days due to higher temperatures


Danger level

1800m
Avalanche Problem
Wind slab
1800m


Caution: fresh snowdrift accumulations.

Snowdrift accumulations which are prone to triggering have been generated particularly in gullies, bowls and behind protruberances in the landscape due to fresh snow and strong to storm-velocity winds. Snowdrifts can be triggered by one single skier and are expected to remain trigger-sensitive. Danger zones occur esp. on shady slopes above 2400m. Avalanches are mostly small-sized. Magnitude and frequency of danger zones will tend to increase with ascending altitude. Be careful of the risks of being swept along and taking a fall.

Snowpack

dp.6: cold, loose snow and wind

As a result of strong winds, trigger-sensitive snowdrift accumulations have been generated esp. in gullies, bowls and behind protruberances in the landscape. The older snowdrifts lie deposited atop soft layers particularly on NW/N/SE facing slopes above 1800m. The old snowpack is faceted, expansively metamorphosed, often weak. The snowpack is highly diverse even over small areas, there is often little snow on the ground below 1600m.

Tendency

Snowdrift accumulations to slowly stabilize over the next few days due to higher temperatures


Danger level



Little snow on the ground. Only isolated avalanche-prone locations.

Avalanches are hardly possible. Isolated danger zones occur on shady slopes and in gullies and bowls. Be careful of the risks of being swept along and taking a fall.

Snowpack

Strong winds are transporting the snow. Locally generally thin snowdrift accumulations will be generated. The drifts lie deposited ato a shallow old snowpack on shady slopes above 1800m. The old snowpack is expansively metamorphosed. There is only little snow on the ground.

Tendency

No change expected in avalanche danger levels