Please note this bulletin is based on limited information. If you have been out and have observations, please send them to [email protected]
Lawinenprobleme
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Likely
Größe
1–3
Wind slabs are widespread and will likely remain sensitive to human triggering, especially on steep convex slopes near ridge crest.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Unlikely - Possible
Größe
1–4
Weak layers deep in the snowpack may become more sensitive to both natural and human triggered avalanches as temperatures increase.
Loose Wet
N
NE
E
SE
S
SW
W
NW
Hochgebirge
Waldgrenze
Unterhalb der Waldgrenze
Wahrscheinlichkeit
Likely
Größe
1–3
Loose wet avalanches may be a concern as cold snow is exposed to warm temperatures for the first time Sunday.
Confidence
Poor - Due to the number of field observations
Weather Forecast
Synopsis: The ridge of high pressure continues to strengthen, driving an inversion pattern across the region that should persist through the forecast period. Sunday: Cloudy with sunny periods. Precipitation: Nil. Alpine temperature: High 1 Light ridge wind. Freezing level: 2400m Monday: Sunny with cloudy periods. Precipitation: Nil. Alpine temperatures: Low -4 High -3 Light ridge wind. Freezing level: 1500 m. Tuesday: Cloudy with sunny periods. Precipitation: Nil. Alpine temperatures: Low 0 High 0 Ridge wind southwest 20 gusting to 65 km/h. Freezing level: 2300 m.
Avalanche Summary
Avalanche activity was reported in pockets of deeper snow from Monday (18th) and Tuesday (19th) in both western and eastern areas of the region. Activity appears to have tapered off. Recent slope tests have produced results only in isolated pockets of wind slab on steep convex rolls.
Snowpack Summary
Treeline snowpack depths in sheltered areas vary between approximately 40-80 cm. In the alpine, coverage is highly variable due to recent high winds. A crust or significant density change may exist around 40 cm below the surface. This has been reported to have weak faceted crystals above and below, and produces sudden "pop" results in compression tests. Below this near the base of the snowpack, an earlier crust buried in October lies close to the ground. This layer may still be of concern on isolated smooth terrain features that have not seen avalanche activity.