Avalanche Forecast

Moderate - Forecast precipitation (either snow or rain) amounts are uncertain. Uncertainty is due to how quickly the snowpack will recover and gain strength.

FRIDAY NIGHT: Cloudy with snowfall, accumulation 10 to 20 cm, 20 to 40 km/h southwest wind, alpine temperature -6 C.

SATURDAY: Cloudy with snowfall, accumulation 2 to 5 cm, 20 to 40 km/h west wind, alpine temperature -6 C, freezing level rising to 1300 m.

SUNDAY: Mix of sun and cloud with no precipitation, 20 to 30 km/h southwest wind, alpine temperature -1 C, freezing level rising to 2000 m.

MONDAY: Cloudy with snowfall, accumulation 5 cm, 30 km/h southwest wind, alpine temperature -4 C, freezing level 1400 m.

May storm and wind slabs were triggered by riders on Thursday to add to the many avalanches observed in the previous few days. Most of the storm slabs released on the surface hoar layer described in the Snowpack Summary, often occurring between around 1600 and 2200 m on all aspects except due south. Read this MIN for a detailed description of a skier-triggered avalanche in the south of the region -- thank you for the detailed report.

Natural and rider-triggered avalanche activity is expected to spike Friday night into Saturday morning during the peak of the storm. Large avalanches are expected to be easily triggered by riders on Saturday in areas where the buried surface hoar described in the Snowpack Summary exists. Avoidance of avalanche terrain, particularly where the surface hoar may exist, is your best bet for having a safe day.

Storm totals may reach 20 to 30 cm by Saturday with locally higher amounts possible. The snow has likely formed new storm slabs in areas sheltered from the wind and wind slabs in exposed terrain at higher elevations from strong south to southwest wind. 

The snow is loading a weak layer of surface hoar crystals 5 to 15 mm in size. Forecast warming may also increase the likelihood of triggering a slab. The layer may be around 40 to 80 cm deep, which is a prime depth for human triggering. The layer is most prominent in areas sheltered from the wind. Example terrain features to treat as suspect include the lee side of protected ridges, openings in the trees, cut blocks, and burns. The layer may not exist on steep sun-exposed slopes, where a melt-freeze crust may be found instead.

The facet/crust layer that formed in early December is buried around 100 to 200 cm. The last reported avalanche was on January 28 in the north of the region. Although unlikely, the layer could be triggered from a large load like a cornice fall or a shallower slab avalanche could step down to this layer. Humans are unlikely to trigger it, with perhaps the exception in thin, shallow snowpack areas. Check out the forecaster blog for more information.

• Travel in alpine terrain is not recommended.
• Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
• Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
• Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.