Avalanche.report

Wednesday 26 March 2025

Published 25 Mar 2025, 17:10:00


Danger level

2400m
Avalanche Problem
Wet snow
2400m
Persistent weak layer
2300m


Caution: wet snow and persistent weak layer

Avalanche danger is moderate. Dry-snow slab avalanches can be triggered by one sole skier above 2300m, the fresh snowdrifts have been deposited also distant from ridgelines in gullies and bowls, avalanches can reach medium size and fracture down to more deeply embedded layers in the snowpack esp. on little-tracked steep north-facing slopes. Small-to-medium moist and dry-snow naturally triggered slab avalanches are possible below 2300m. Wet-snow avalanches in extremely steep terrain and isolated glide-snow avalanches can be expected, mostly small releases.

Snowpack

Due to reduced nocturnal outgoing longwave radiation the snowpack surface can hardly cool and rapidly softens in the early morning hours. The snowpack is moist in all aspects up to high altitudes. On shady slopes at high and high-alpine altitudes the freshly generated foehn-induced drifts lie deposited atop an unfavorable snowpack surface. Inside the old snowpack are several weak layers of faceted crystals which can serve as a slab atop the fresh snowdrifts. Also on sunny slopes, moist slabs can slide away over the uppermost crusts of the old snowpack.

Tendency

Little change expected


Danger level

2400m
Avalanche Problem
Wet snow
2400m


Wet loose-snow avalanches in very steep terrain are the main danger

Avalanche danger is low. Isolated small loose-snow naturally triggered avalanches are possible or can be triggered by one sole skier. Danger zones for small slab avalanches in the snowdrifts occur seldom on very steep north-facing slopes at high altitudes. On steep grass-covered slopes, isolated small glide-snow avalanches are possible. Apart from the danger of being buried in snow masses, the risks of being swept along and forced to take a fall demand adequate consideration.

Snowpack

Due to reduced nocturnal outgoing longwave radiation the snowpack surface can hardly cool and rapidly softens in the early morning hours. The snowpack is moist in all aspects up to high altitudes. At high altitudes the old snowpack fundament on shady slopes is often poor, but the requisite slab is lacking.

Tendency

Little change expected