Avalanche Forecast
Issued: Feb 5th, 2021 4:00PM
The alpine rating is Persistent Slabs and Wind Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeContinued discipline and careful route finding will be required on Saturday to avoid triggering large avalanches on a buried persistent weak layer of surface hoar. This layer has been especially reactive at treeline elevations.
Summary
Confidence
Moderate - Uncertainty is due to the limited number of field observations.
Weather Forecast
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FRIDAY NIGHT: Cloudy / Strong, northwest ridgetop wind / alpine low temperature -16 / Freezing level valley bottom.
SATURDAY: Cloudy with flurries; 3-10 cm. / Moderate, west ridgetop wind / alpine high temperature -7 / Freezing level valley bottom.
SUNDAY: Mix of sun and cloud / Moderate, northwest ridgetop wind / alpine high temperature -12 / Freezing level valley bottom.
MONDAY: Sunny / Light, northwest ridgetop wind / alpine high temperature -13 / Freezing level valley bottom.
Avalanche Summary
There was a recent report of skier remotely triggering a size 2.5 persistent slab from a ridgetop at treeline near Quartz Creek on Wednesday. This avalanche failed on the very weak layer of surface below the recent storm snow. It was reported that light wind effect had stiffened the recent storm snow just enough to be highly reactive to skier triggering. Min report HERE.
Touchy storm slabs are sitting on a weak layer of surface hoar which is likely to be reactive to human triggers. Avalanches may be larger than expected due to the presence of this weak layer.
Snowpack Summary
Southwest switching to northwesterly winds may form reactive wind slabs on a variety of aspects at treeline and above.
40-60 cm. of recent snow is sitting on a very weak layer of surface hoar which has potential to surprise backcountry users by how easily it may be triggered and how wide the persistent slabs propagate across slopes. Recent avalanches on this layer have primarily been reported at treeline and below.
60-100 cm. down is an older surface hoar and/or a thin melt crust from mid January. This layer was more prominent in the north Purcells in sheltered, open slopes at treeline.
Deep persistent weak layers can still be found in the lower snowpack. These weak layers are most likely to be triggered from rocky areas with a shallow or thin to thick snowpack.
Terrain and Travel
- Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
- Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
- Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
- Be careful as you transition into wind affected terrain.
- Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
Problems
Persistent Slabs
40-60 cm of recent snow has formed reactive slabs sitting on a persistent weak layer of surface hoar. These slabs may be especially reactive in wind affected terrain.
Aspects: All aspects.
Elevations: Treeline, Below Treeline.
Likelihood
Expected Size
Wind Slabs
Southwest switching to northwesterly winds may form reactive wind slabs on a variety of aspects at treeline and above.
Aspects: North, North East, East, South East, South.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Valid until: Feb 6th, 2021 4:00PM