Avalanche.report

Monday 24 March 2025

Published 25 Mar 2025, 09:44:00


Danger level

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


Wet-snow problem up to high altitudes. Above 2300m: hidden 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 isolaated glide-snow avalanches can be expected, mostly small release (loose-snow, slabs gliding over the ground atop a melt-freeze crust).

Snowpack

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. Due to reduced nocturnal outgoing longwave radiation and solar radiation during daytime hours, the snowpack is at least moist up to 2300m and is rapidly forfeiting its firmness.

Tendency

Likelihood of the snowdrifts triggering will gradually decrease, wet-snow problem and persistent weak layer will continue.


Danger level


Avalanche Problem
Wet snow


Danger of falling outweighs that of being buried in snow masses

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 N/E facing slopes at high altitudes. On steep grass-covered slopes, isolated small glide-snow avalanches are possible.

Snowpack

The shallow, generally stable snowpack has consolidated well. On shady slopes, thin fresh snowdrift accumulations are being generated. Due to reduced nocturnal outgoing longwave radiation and often diffuse radiation the snowpack is superficially moist and forfeiting its firmness.

Tendency

Little change expected