Snowdrifts more trigger prone with ascending altitude. Smaller wet snow avalanches possible at all altitudes.
Avalanche danger above 1800 m is moderate, below that altitude danger is low. Older snowdrifts can be a problematic. In places, slabs can be triggered even by small additional loading. Avalanche prone locations are found in particular in steep ridgeline terrain at high altitude in east and south aspects as well as in wind-loaded gullies and bowls. Snowpack In addition,small wet loose snow avalanches can release naturally in very steep terrain. Isolated glide snow avalanches that are mostly small are possible on steep smooth grass-covered slopes. At intermediate altitudes this applies to all aspects; at high altitudes it appplies to sun-exposed slopes.
Snowpack
In particular at high altitudes soft layers under and within small-scale snowdrifts are still prone to triggering. There are still isolated layers consisting of faceted crystals in the are of crusts; they are still triggerable. Due to warming, the snow is thoroughly moist at intermediate altitudes and on the sunny side at high altitudes. Due to clear skies during Monday night, a melt-freeze crust will form in places that will soften again during the day. At higher altitudes moistening continues also on Tuesday; frequently the snowpack is wet down to the ground. Snow depths varies; all in all there is little snow.
Tendency
Thanks to mild weather snowdrift problem will decrease Wet and gliding snow problem will remain.
Danger level
Avalanche Problem
Wet snow
Gliding snow
Minor glide snow avalanches and sluffing can occur.
Avalanche danger is low. Main problem: wet snow. In isolated cases on very steep slopes where the ground is smooth, small glide-snow avalanches can unleash spontaneously. Isolated glide snow avalanches that are mostly small are possible on steep smooth grass-covered slopes.
Snowpack
The snowpack is thoroughly moist down to deep layers. Monday night will see mostly clear skies, in free terrain a melt-freeze crust will form that is capable of bearing loads which softens again during the day. As a consequence it forfeits its firmness. Often the snowpack is wet where it borders the ground, i.e. it can start sliding over soft ground. Snow depths vary. Ridges and crests are blown bare; south-facing slopes are becoming increasingly bare. All in all, there is still little snow.