Avalanche.report

Tuesday 14 January 2025

Published 13 Jan 2025, 17:00:00


Danger level

2000m
Avalanche Problem
Wind slab
2000m


Favorable conditions. Caution: small-area snowdrift accumulations

Avalanche danger at high altitudes is moderate, danger below that altitude is low. In ridgeline terrain, in gullies and bowls, freshly generated snowdrift accumulations require caution. They are mostly small-sized, but poorly bonded with the old snowpack and thus, prone to triggering. In risky terrain for falls, evaluate the drifts with caution, small-sized - avalanches can be triggered by one sole skier. Glide-snow avalanches still possible.

Snowpack

The lastest round of fresh snowfall has been deposited as loose-snow following the lower temperatures atop a well consolidated, often encrusted old snowpack surface. In high altitude ridgeline terrain it was often transported, thus generating small-area drifted masses. Not much snow on the ground at low altitudes.

Tendency

Avalanche danger levels will continue to diminish


Danger level

2000m
Avalanche Problem
Wind slab
2000m


Generally favorable conditions, moderate avalanche danger

Small-area fresh and older trigger-sensitive snowdrift accumulations are the main danger. Danger zones occur in wind-loaded steep terrain, in gullies and bowls, and behind protruberances in the landscape. Size and frequency of danger zones tend to increase with ascending altitude. In addition, on steep shady slopes at high altitudes and in transitions from shallow to deep snow, isolated slab avalanches can be triggered by large additional loading. A cautious route selection is advised. Small-to-mediium glide-snow avalanches are possible only in isolated cases. Caution urged below glide cracks.

Snowpack

The lastest round of fresh snowfall has been deposited as loose-snow following the lower temperatures atop a well consolidated, often encrusted old snowpack surface, but fresh drifts tend to be often poorly bonded with the old snowpack surface with ascending altitude, sometimes will buried layers of graupel. More deeply embedded layers in the old snowpack are hardly prone to triggering. At most, where the snow is shallow and on very steep shady slopes.

Tendency

No significant change expected, caution urged towards high altitude snowdrifts