The recent snow has added load to buried weak layers and may still be reactive to human triggers. Conservative terrain selection is recommended.
Avalanche problems
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible
Size
1–2
Recent snow may have been redeposited with southwest winds that switched to northeast winds. The touchiest pockets will likely be adjacent to ridges.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Possible - Likely
Size
1.5–2.5
40 to 60 cm of snow is loading a weak layer of feathery surface hoar crystals, which is best preserved in shaded and sheltered areas between 1600 m and 1900 m. On southerly aspects, the snow sits on a hard melt-freeze crust. This layer may be touchy.
Deep Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Unlikely - Possible
Size
2–3.5
The bottom of the snowpack consists of weak and sugary faceted snow. The consequences of triggering this layer remains high, as avalanches will be large and destructive.
Confidence
Moderate -
Weather Forecast
MONDAY NIGHT - Clear with cloudy periods / northeast winds 10-15 km/h / alpine low temperature near -20TUESDAY - A mix of sun and cloud / northeast winds 10-15 km/h / alpine high temperature near -18WEDNESDAY - Mainly sunny / northeast winds 15-25 km/h / alpine high temperature near -16THURSDAY - A mix of sun and cloud / southwest winds, 15-35 km/h / alpine high temperature near -13
Avalanche Summary
No new avalanches were reported on Sunday.Many small to large avalanches were triggered within the recent storm snow by skiers, naturally, and explosives on Saturday. The fact that we have numerous weak layers within our snowpack indicates that conservative decisions should be made at this time.
Snowpack Summary
Above 1700 m, 30 to 40 cm of recent snow overlies a variety of surfaces, including feathery surface hoar crystals in shaded and sheltered areas, wind-affected snow in exposed terrain, and a melt-freeze crust on southerly aspects. Below 1700 m, expect to find around 5-10 cm of low-density snow on a melt-freeze crust.The mid-January layer of surface hoar or a crust is buried around 40 to 60 cm. The surface hoar is found on shaded and sheltered slopes and is most prominent between 1600 m and 1900 m but has been found up to 2100 m. The melt-freeze crust is found on south aspects at all elevations.The middle of the snowpack is generally consolidated. The bottom half of the snowpack is unconsolidated and composed of weak and sugary faceted grains.