Avalanche danger above the treeline is considerable, below that altitude danger is low. Snowdrift accumulations above the treeline can be easily triggered even by one single winter sports enthusiast and grow to medium size. Slab avalanches can often fracture down to more deeply embedded layers inside the snowpack and grow to large size. Danger zones occur particularly behind protruberances in the landscape, in gullies and blows and on wind-loaded slopes. These have been covered by fresh snow in many places, making them difficult to recognize. Whumpf noises and glide-cracks when the snowpack is stepped on are signals of danger. At low and intermediate altitudes on steep grass-covered slopes, small glide-snow avalanches are possible.
Snowpack
Since yesterday there has been 40-45cm of fresh snow registered in the barrier cloud regions, elsewhere 25-30cm. Due to strong-to-storm strength W/NW winds there has been wide-reaching transport. During the daytime due to brisk-to-strong NW winds, and tomorrow W/SW winds, additional trigger-sensitive snowdrift accumulations have been generated and will continue to be. The drifts lie deposited atop a weak old snowpack on high-altitude shady slopes, on sunny slopes often atop a thin melt-freeze crust. Weak layers can occur on high altitude slopes where the old snowpack was previously loose and also inside the snowdrifts themselves. During the daytime, in addition, graupel showers will pass through. At low altitudes the fresh snow and drifts lie deposited atop a moistened old snowpack surface with better consolidation.
Tendency
Following a brief improvement in weather conditions on Saturday, renewed preciptiation will set in during Saturday night, accompanied by strong-to-storm strength W/NW winds. Avalanche danger levels are expected to increase significantly over widespread areass.
Avalanche danger above the treeline is moderate, below that altitude danger is low. Snowdrift accumulations above the treeline can be triggered by one single skier and in isolated cases grow to medium size. Danger zones occur especially behind protruberances in the landscape, in gullies and bowls, and on wind-loaded slopes. Size and frequency of these avalanche prone locations tend to increase with ascending altitude. They have been blanketed in some places, making them difficult to recognize. Below the treeline avalanche danger is low. At low altitudes small glide-snow avalanches are possible on steep grass-covered slopes.
Snowpack
Since yesterday there has been 25-30cm of fresh now registered. Due to strong-to-storm strength W/NW winds there has been wide-reaching transport. During the daytime due to brisk-to-strong NW winds, and tomorrow W/SW winds, additional trigger-sensitive snowdrift accumulations have been generated and will continue to be. The drifts lie deposited atop a weak old snowpack on high-altitude shady slopes, on sunny slopes often atop a thin melt-freeze crust. Weak layers can occur on high altitude slopes where the old snowpack was previously loose and also inside the snowdrifts themselves. During the daytime, in addition, graupel showers will pass through. At low altitudes the fresh snow and drifts lie deposited atop a moistened old snowpack surface with better consolidation.
Tendency
Following a brief improvement in weather conditions on Saturday, renewed precipitation will set in during Saturday night, accompanied by strong-to-storm strength W/NW winds. Avalanche danger levels are expected to increase significantly over widespread areass.
