Avalanche Forecast

Issued: Mar 9th, 2021 4:00PM

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

Avalanche Canada JSmith, Avalanche Canada

Lingering wind slabs may remain reactive on steep, convex slopes below alpine ridgetops. A persistent slab problem may still be possible to trigger in isolated areas in the north of the region and warrants continued consideration.

Summary

Confidence

High - Confidence is due to a stable weather pattern with little change expected.

Weather Forecast

 TUESDAY NIGHT: Increasing cloudiness / Moderate, west ridgetop wind / alpine low temperature -12 / Freezing level valley bottom.

WEDNESDAY: Cloudy with flurries; 2-5 cm. / Light, southwest ridgetop wind / alpine high temperature -5 / Freezing level 1300 m.

THURSDAY: Sunny / Moderate, northwest ridgetop wind / alpine high temperature -4 / Freezing level 1400 m.

FRIDAY: Sunny / Moderate, northwest ridgetop wind / alpine high temperature -1 / Freezing level 1700 m.

Avalanche Summary

There was a MIN report on Monday of a small wet loose point release triggering a size 2 slab avalanche around 30 cm. deep on a south aspect. See MIN HERE.

Last week there were several notable reports of large human triggered persistent slab avalanches in the Dogtooth Range and Quartz Creek area. See these MIN reports here and here. The likelihood of triggering on these layers has since gone down, but it's still worth considering the potential for a similar release to occur.

Snowpack Summary

Dry soft snow can be found on shaded aspects above around 1500 m. On south-facing slopes and at lower elevations expect crusty snow in the morning and soft moist snow in the afternoon. Recent wind slabs and cornices still pose a hazard close to steep ridgelines.

Persistent weak layers were reactive last week, particularly in the northern end of the Purcells. The layers of concern are a buried layer of surface hoar that formed in late January is 30-60 cm deep and an older surface hoar layer is 50-100 cm deep at treeline. These layers may exist as a combination of facets and crusts at other elevations. Recent assessments indicate the chance of triggering these layers has reduced, but writing them off completely is probably premature.

Shallow rocky areas where the snowpack is thin likely have sugary facets acting as a weak layer at the base of the snowpack.

Terrain and Travel

  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • Caution around slopes that are exposed to cornices overhead.

Problems

Wind Slabs

An icon showing Wind Slabs

Lingering wind slabs may remain reactive to human triggers on steep, convex slopes below ridgetops.

Aspects: North, North East, East, South East, North West.

Elevations: Alpine.

Likelihood

Possible

Expected Size

1 - 2

Persistent Slabs

An icon showing Persistent Slabs

Persistent slab avalanches remain possible in the northern tip of the Purcells where there has been recent avalanche activity on a 40-80 cm deep layer of surface hoar, facets, and/or crusts (see Avalanche Summary).

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Unlikely

Expected Size

2 - 3

Valid until: Mar 10th, 2021 4:00PM