Allgäu Alps Central

Beware snowdrifts behind discontinuities in the terrain, also distant from ridges

Beware snowdrifts behind discontinuities in the terrain, also distant from ridges

Avalanche danger above 2000 m is considerable, below that altitude danger is moderate. Main problem: snowdrift accumulations. Danger zones occur in steep ridgeline terrain on N/E/SW facing slopes, behind discontinuities in the terrain and in wind-loaded gullies and bowls, releases small-to-medium sized. Slabs can be triggered by 1 person, e.g. a skier. In isolated cases small glide-snow avalanches are possible on steep grass-covered slopes, releases can be large. Solar radiation triggering moistly small loose-snow avalanches in steep rocky terrain naturally.

Stormy westerly winds have transported the fresh snow and generated new snowdrift accumulations. Inside the drifts are trigger-prone layers. In transitions to the old snowpack at high altitudes a weak faceted layer has formed at high altitudes due to low temperatures. The proneness to triggering increases with ascending altitude. Beneath a melt-freeze crust in the uppermost part of the snowpack is a wet layer which can be triggered in some areas. Elsewhere the old snowpack is compact and stable; thoroughly moist and wet down to the ground. Also the fresh fallen snow will moisten through warmth and solar radiation on Monday, forfeiting its bonding, possibly triggering as loose snow.

Persistent warmth on Tuesday will further consolidate the snowdrifts, danger will recede somewhat.