All the recent snow is of concern because 1) it may not bond well to underlying layers and 2) it is loading buried weak layers. Conservative decision-making is essential!
Avalanche problems
Wind Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
Likely
Size
1–2
Recent snow may have been redeposited with southwest winds in exposed terrain. The touchiest pockets will likely be in lee terrain features adjacent to ridges.
Persistent Slabs
N
NE
E
SE
S
SW
W
NW
Alpine
Treeline
Below treeline
Likelihood
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 - Intensity of incoming weather systems is uncertain
Weather Forecast
SATURDAY NIGHT: Cloudy with light snowfall, accumulation 5 to 10 cm, cooling overnight.SUNDAY: Cloudy with light snowfall, accumulation 5 to 10 cm, light southwest winds, alpine temperature -27 C.MONDAY: Cloudy with light snowfall, accumulation 5 cm, light north winds, alpine temperature -29 C.TUESDAY: Mostly clear skies, light north winds, alpine temperature -18 C.
Avalanche Summary
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 to 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.