Storm slab problems vary by elevation band. Wind loading patterns are your guide to avoiding slabs at higher elevations. Further down, carefully manage steep, sheltered slopes that may harbour surface hoar.
Avalanche Problem 1: Storm Slabs




- Sheltered openings at mid elevations are likely areas for surface hoar to be preserved.
- Use ridges or ribs to avoid steep pockets of wind loaded snow at higher elevations.
- Avoid steep convex rolls in sheltered openings at mid elevations.
Avalanche Summary
Reports from Friday included observations of numerous older storm slab releases that occurred during last week's storm. These reached to Size 2.5 and were focused on terrain around a 38 degree incline. Both north and south aspects were active. Another older Size 2.5 persistent slab release was also noted. This slab was about 80 cm thick, failed on a low elevation moraine feature on a north aspect, and is suspected to have run on the weak layer from late December.
Reports from Thursday included observations of several storm slabs releasing naturally, remotely (from a distance), and with skier traffic. Avalanche sizes ranged from Size 1-2. The remote release was noted to have slid on lower angle terrain over a surface hoar on crust 'combo' left behind by the recent inversion.
Looking forward, the recent storm snow is expected to become generally more stable, except where it overlies pockets of surface hoar and where wind -affected. Surface hoar is more likely to exist in sheltered openings at mid elevations. Wind slabs at ridgecrests and around exposed terrain features are an increasing concern.
Snowpack Summary
Last week's storm brought about 30 cm of new snow to the region. Northern parts of the region saw about half this amount. The new snow buried a mix of old wind slabs and temperature crusts left over from last weekend. More isolated surface hoar has been observed under the new snow at mid elevations that experienced cloud cover during recent inversion conditions. Storm slabs have been particularly reactive where this surface hoar exists.
Professionals have been monitoring a few layers in the upper snowpack, including crusts and surface hoar layers buried 40-80 cm below the surface. Although these layers have been reactive in recent snowpack tests, only one recent report exists of a persistent slab releasing over the late December weak layer. The lower snowpack is generally strong, with the exception of areas around Stewart and further north where a basal crust and facets exist.
Weather Forecast
Saturday night: Flurries bringing approximately 5 cm of new snow. Moderate to strong southeast winds.
Sunday: Cloudy with continuing scattered flurries bringing 2-4 cm of new snow. Light variable winds. Alpine high temperatures around -7.
Monday: Cloudy with flurries bringing 5-10 cm of new snow, continuing overnight. Light to moderate southwest winds. Alpine high temperatures around -7.
Tuesday: Mainly cloudy with isolated flurries and a trace of new snow, increasing overnight. Strong southeast winds. Alpine high temperatures of -6.
Avalanche Forecasts in your Inbox
Avalanche Canada has switched to an RSS feed for its daily forecasts. This is a much more flexible method that allows automatic delivery to your email inbox, or to an RSS reader of your choice.
What are RSS feeds?
RSS (Really Simple Syndication) is a popular standardized file format allowing up-to-date delivery of web-based content. RSS feeds enable you to receive content updates from websites, delivered to your email through an RSS aggregator (such as blogtrottr.com) or viewed through applications called RSS readers (such as feedly.com).
Set up an RSS feed for your email:
Select a RSS aggregator
- Northwest Coastal URL:
http://www.avalanche.ca/api/forecasts/northwest-coastal.rss - Copy the url and paste it into the appropriate field of your RSS aggregator.
- Fill in your email address.
- Voila! Watch the Avalanche Canada forecast roll into your inbox.
Forecast Disclaimer
Avalanche Canada's Public Avalanche Bulletin, and other information and services provided by Avalanche Canada, are intended for personal and recreational purposes only.
**THIS INFORMATION IS PROVIDED "AS IS" AND IN NO EVENT SHALL THE PROVIDERS BE LIABLE FOR ANY DAMAGES, INCLUDING, WITHOUT LIMITATION, DAMAGES RESULTING FROM DISCOMFORT, INJURY, OR DEATH, CLAIMS BY THIRD PARTIES OR FOR OTHER SIMILAR COSTS, OR ANY SPECIAL, INCIDENTAL, OR CONSEQUENTIAL DAMAGES, ARISING OUT OF THE USE OF THE INFORMATION.**
The user acknowledges that it is impossible to accurately predict natural events such as avalanches in every instance, and uses the data in this bulletin with this always foremost in mind. The accuracy or reliability of the data is not guaranteed or warranted in any way and the Providers disclaim liability of any kind whatsoever, including, without limitation, liability for quality, performance, merchantability and fitness for a particular purpose arising out of the use, or inability to use the data.
Recent snowfall has buried widespread temperature crusts and more isolated surface hoar. Surface hoar may be found around sheltered mid elevations. At higher elevations, watch for wind slabs in the lee of ridgecrests and exposed terrain features.