30-60 cm of recent new snow has been redistributed by recent north and east winds.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alta montaña
Límite del bosque
Bajo el límite del bosque
Probabilidad
Possible
Tamaño
1–2.5
50-90 cm of snow now sits on a weak layer of surface hoar and crust that was buried in mid January. This layer has been most reactive at lower elevations.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alta montaña
Límite del bosque
Bajo el límite del bosque
Probabilidad
Unlikely - Possible
Tamaño
3–4
The base of the snowpack has a very weak layer that continues to produce very large avalanches from time to time. The probability of triggering this layer is somewhat low, but the consequences are very high.
Confidence
High - The weather pattern is stable
Weather Forecast
FRIDAY - Mix of sun and cloud / light to moderate east wind / alpine temperature -18SATURDAY - Mainly sunny / moderate east wind / alpine high temperature near -20SUNDAY - Mix of sun and cloud / light east wind / alpine temperature -15
Avalanche Summary
A persistent weak layer that was buried in mid January continues to be reactive to human triggers. This layer is sensitive enough to trigger remotely (from a distance). Human triggered avalanches up to size 2 were reported on Sunday and Monday. This MIN report from Sunday illustrates the potential for humans to remotely trigger the mid January layer.
Snowpack Summary
Approximately 30-60 cm of recent new snow sits on wind slab, surface hoar (feathery crystals), facets (sugary snow) and a crust on sun-exposed slopes. A very notable feature in the snowpack at this time is a persistent weak layer that was buried in mid January, which is now buried 50-90 cm. This layer consists primarily of surface hoar, however there is also a crust associated with it on sun-exposed slopes. This layer has been most reactive at treeline and below.The base of the snowpack has a deep persistent weak layer near the ground. This layer consists of facets over a crust. This weak interface continues to produce large and destructive avalanches that are sporadic in nature, and very difficult to predict. This layer is most likely to be triggered from areas where the snowpack is shallow and weak. Rocky alpine bowls, ridge crests and rocky outcroppings are some examples of the kind of terrain to be wary of.