Avalanche Forecast Purcells

Date Issued: Valid Until:

Avalanche Canada mbender, Avalanche Canada

Avalanche Forecast

Thu Feb. 7th ยท 4:44PM

Alpine

Danger Ratings Moderate

Treeline

Danger Ratings Considerable

Below Treeline

Danger Ratings Considerable
Persistent Slabs Persistent Slabs
Wind Slabs Wind Slabs
Deep Persistent Slabs Deep Persistent Slabs

Alpine

Danger Ratings Moderate

Treeline

Danger Ratings Considerable

Below Treeline

Danger Ratings Considerable

Alpine

Danger Ratings Moderate

Treeline

Danger Ratings Considerable

Below Treeline

Danger Ratings Considerable
There is potential for triggering large avalanches treeline and below due to the presence of a persistent slab problem. Click here to see our Forecasters' Blog for a more detailed description of current conditions.

Confidence

High - The weather pattern is stable

Weather Forecast

FRIDAY - Mix of sun and cloud / light to moderate east wind / alpine temperature -18SATURDAY - Mainly sunny / moderate east wind / alpine high temperature near -20SUNDAY - Mix of sun and cloud / light east wind / alpine temperature -15

Avalanche Summary

A persistent weak layer that was buried in mid January continues to be reactive to human triggers. This layer is sensitive enough to trigger remotely (from a distance). Human triggered avalanches up to size 2 were reported on Sunday and Monday. This MIN report from Sunday illustrates the potential for humans to remotely trigger the mid January layer.

Snowpack Summary

Approximately 30-60 cm of recent new snow sits on wind slab, surface hoar (feathery crystals), facets (sugary snow) and a crust on sun-exposed slopes. A very notable feature in the snowpack at this time is a persistent weak layer that was buried in mid January, which is now buried 50-90 cm. This layer consists primarily of surface hoar, however there is also a crust associated with it on sun-exposed slopes. This layer has been most reactive at treeline and below.The base of the snowpack has a deep persistent weak layer near the ground. This layer consists of facets over a crust. This weak interface continues to produce large and destructive avalanches that are sporadic in nature, and very difficult to predict. This layer is most likely to be triggered from areas where the snowpack is shallow and weak. Rocky alpine bowls, ridge crests and rocky outcroppings are some examples of the kind of terrain to be wary of.

Problems

Persistent Slabs

Persistent Slabs

50-90 cm of snow now sits on a weak layer of surface hoar and crust that was buried in mid January. This layer has been most reactive at lower elevations.

Any steep opening in the trees should be treated as suspect right now.Choose low angled terrain.

Aspects: All aspects.

Elevations: Treeline, Below Treeline.

Likelihood

Possible

Expected Size

1 - 2.5
Wind Slabs

Wind Slabs

30-60 cm of recent new snow has been redistributed by recent north and east winds.

If triggered, wind slabs may step down to deeper layers and result in large avalanches.Be careful with wind loaded pockets, especially near ridge crests and roll-overs.

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

Elevations: Alpine.

Likelihood

Possible - Unlikely

Expected Size

1 - 2
Deep Persistent Slabs

Deep Persistent Slabs

The base of the snowpack has a very weak layer that continues to produce very large avalanches from time to time. The probability of triggering this layer is somewhat low, but the consequences are very high.

Minimize overhead exposure; avalanches triggered by cornice fall may be large and destructive.Use caution on alpine slopes, especially around thin areas that may propagate to deep instabilities.Avoid making assumptions about this layer based on aggressive tracks on adjacent slopes.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible - Unlikely

Expected Size

3 - 4