Avalanche report

Avalanche danger is MODERATE. Due to solar radiation and diffuse light, natural releases (loose dry and loose moist) are to be expected in extremely steep terrain (>40°). Small releases by 1 person are possible. Fresh ridgeline snowdrifts can be triggered as a small slab even by 1 person. Danger zones occur on steep slopes (over 35°) on north facing slopes. Fresh ridgeline snowdrifts can be triggered as a small slab by 1 person, danger zones occur on very steep north-facing slopes. Where snow is sufficient below 2600 m, small glide-snow avalanches can release naturally, esp. where recent snowfall fell on bare ground. Avoid zones below glide cracks.

Loose snow on the surface can lose bonding through solar radiation, but radiation also helps the snowpack to settle. Weak layers in the uppermost part of the snowpack (blanketed fresh snow and graupel). In transitions from the old snowpack to the fresh snow there are graupl and facted layers above 2400 m, not easily triggerable. Reserves of cold are limited to shady slopes above 2600 m. Atop snowy steep rocks and grassy slopes the snowpack is wet at ground level and can glide away.

Due to higher temperatures the snowpack will moisten, the wet-snow problem will increase.

Avalanche danger is MODERATE. Where snow is sufficient, small glide-snow avalanches can release naturally cases in extremely steep terrain (>40°), especially where the ground was previously bare of snow. Avoid zones below glide cracks. Loose-snow avalanches can in isolated cases in extremely steep terrain (>40°) release naturally or by 1 person due to radiation, releases small.

Loose snow on the surface can lose bonding through solar radiation, but radiation also helps the snowpack to settle. Blanketed fresh snow or graupel can be a near-surface weak layer. As a result of solar radiation, bonding is generally good. Atop snowy steep rocks and grassy slopes the snowpack is wet at ground level and can glide away.

Due to higher temperatures the snowpack will moisten, the wet-snow problem will increase.

Avalanche danger is MODERATE. Due to solar radiation and diffuse light, natural releases (loose dry and loose moist) are to be expected in extremely steep terrain (>40°). Small releases by 1 person are possible. Where snow is sufficient below 2600 m, small glide-snow avalanches can release naturally, esp. where recent snowfall fell on bare ground. Avoid zones below glide cracks. Fresh ridgeline snowdrifts can be triggered as a small slab even by 1 person. Danger zones occur on steep slopes (over 35°) on north facing slopes.

Loose snow on the surface can lose bonding through solar radiation, but radiation also helps the snowpack to settle. Weak layers in the uppermost part of the snowpack (blanketed fresh snow and graupel). In transitions from the old snowpack to the fresh snow there are graupl and facted layers above 2400 m, not easily triggerable. Reserves of cold are limited to shady slopes above 2600 m. Atop snowy steep rocks and grassy slopes the snowpack is wet at ground level and can glide away.

Due to higher temperatures the snowpack will moisten, the wet-snow problem will increase.

Avalanche danger is low. Due to solar radiation and diffuse light, natural releases (loose dry and loose moist) are to be expected in extremely steep terrain (>40°). Small releases by 1 person are possible. Fresh snowdrift accumulations in high altitude ridgeline terrain are small, can trigger a small slab. Danger of falling outweighs that of snow masses.

Loose snow on the surface can lose bonding through solar radiation, but radiation also helps the snowpack to settle. Blanketed fresh snow or graupel can be a near-surface weak layer. As a result of solar radiation, bonding is generally good. Bonding is generally good, the base is compact.

Due to higher temperatures the snowpack will moisten, the wet-snow problem will increase.