Avalanche Forecast

Issued: Mar 7th, 2019 4:27PM

The alpine rating is moderate, the treeline rating is moderate, and the below treeline rating is low. Known problems include Storm Slabs and Persistent Slabs.

Avalanche Canada kdevine, Avalanche Canada

Fresh storm slabs may be reactive to human triggering. Watch for signs of instability such as whumphing, cracking and recent avalanches.

Summary

Confidence

Moderate -

Weather Forecast

THURSDAY NIGHT - Mainly cloudy with isolated flurries, 5-10 cm / southwest winds 20-40 km/h / alpine low temperature near -13FRIDAY - Mainly cloudy with isolated flurrie, up to 5 cm / southwest winds 10-25 km/h / alpine high temperature near -11SATURDAY - A mix of sun and cloud / northwest winds 10-15 km/h / alpine high temperature near -12SUNDAY - Sunny with cloudy periods / northwest winds 10-15 km/h / alpine high temperature near -9

Avalanche Summary

On Wednesday, a size 2 persistent slab avalanche was triggered by a cornice failure on a southeast aspect in the alpine. This avalanche reportedly failed on the late-January persistent weak layer.Observations from the past few days have shown size 1-2 wind slabs releasing with skier traffic on a range of aspects in the alpine and at treeline. Small (size 1-1.5) loose dry avalanches have also been observed releasing naturally from steeper, sun exposed slopes. Persistent slab avalanche activity on the three buried surface hoar layers (described in more detail in the Snowpack Summary) has slowed down, but not stopped. This has evolved into a low likelihood avalanche/high consequence avalanche problem at treeline and below.

Snowpack Summary

10-20 cm of new snow is sitting on wind slabs, surface hoar (feathery crystals) and facets (sugary snow), and a crust on sun exposed slopes. The buried wind slabs are also sitting on facets and may continue to be reactive.There are three prominent weak layers in the upper snowpack that were buried in mid and late January, and early February. They can be found between 30-90 cm below the surface. These layers consist primarily of surface hoar, though they may be associated with crusts on steeper, south facing slopes. These weak layers are most prominent at lower elevations - especially below treeline. The lower snowpack is generally considered to be strong, except for shallow, rocky areas where the cold temperatures continue to facet (weaken) the snowpack.

Problems

Storm Slabs

An icon showing Storm Slabs
Fresh storm slabs may be reactive, especially in wind loaded areas.
Avoid wind loaded pockets near ridge crests and back off from slopes that feel hollow or drum-like.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 1.5

Persistent Slabs

An icon showing Persistent Slabs
Three persistent weak layers are buried between 30-90 cm. These layers have evolved into a lower likelihood/high consequence avalanche problem.
Exercise increased caution around low elevation cut-blocks where this layer has been well preserved.

Aspects: All aspects.

Elevations: Treeline, Below Treeline.

Likelihood

Unlikely

Expected Size

1 - 2

Valid until: Mar 8th, 2019 2:00PM