New snow fell in the south of the region, which will produce new storm slabs and load buried weak layers. Conservative decision-making is recommended, as large avalanches are likely.
Avalanche Problem 1: Persistent Slabs




- Use extra caution in open trees and sheltered features where surface hoar may be preserved.
- Be aware of the potential for large, destructive avalanches due to buried surface hoar.
Avalanche Problem 2: Storm Slabs




New snow fell in the south of the region, producing fresh slabs that overly previous storm and wind slabs. Observe for signs of instability, such as cracking, whumpfing, and avalanche activity.
- If triggered, storm slabs may step down to deeper layers, resulting in large avalanches.
- Approach lee and cross-loaded slopes with caution.
- Be aware of the potential for loose dry avalanches in steep terrain where snow hasn't formed a slab.
Avalanche Summary
On Wednesday, large (size 2.5) persistent slab avalanches were reported in the region at alpine and treeline elevations, being remotely triggered (from a distance), 50 to 150 cm deep, and on northeasterly aspects. Similarly, large (size 2) storm slabs were explosively controlled near Terrace on easterly to northeasterly aspects, with slab depths of 40 to 75 cm, at elevations around 1200 to 1350 m. Loose dry avalanches were also explosively controlled on easterly aspects.
On Tuesday, numerous large (size 2-3) persistent slabs released remotely on a layer of surface hoar buried 40-60 cm deep in the Terrace area. This activity was focused on shaded aspects at treeline and below treeline elevations.
Snowpack Summary
Thursday's storm is expected to bring another 10 to 30 cm of snow to the southern parts of the region. This overlies last weekends 50 to 80 cm of storm snow, with the highest accumulation at high elevations and closest to the coast. Strong westerly winds have redistributed last weeks snow in open areas.
Two layers of surface hoar exist in the region at depths of about 40 to 60 cm, being buried early and mid-March. At low elevations, a melt-freeze crust also exists.
Numerous dormant layers exist deeper in the snowpack. Layers of crusts, facets, and isolated surface hoar buried 50 to 100 cm exist from mid- and late-February. A surface hoar/crust layer from January is buried around 150 to 200 cm. Near the bottom of the snowpack, weak and sugary facets exist in colder and dryer parts of the region, such as the far north.
Weather Forecast
THURSDAY NIGHT: Cloudy with snowfall, accumulation 5 to 10 cm, moderate southwesterly winds, alpine temperature -6 C, freezing level 500 m.
FRIDAY: Mostly cloudy, light northwesterly winds, alpine temperature -5 C, freezing level 800 m.
SATURDAY: Mostly cloudy, light southwesterly winds, alpine temperature -6 C, freezing level 700 m.
SUNDAY: Mostly cloudy, light southwesterly winds, alpine temperature -7 C, freezing level 400 m.
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.
A weak surface hoar layer buried about 50 cm has produced large slab avalanches that have propagated widely. It is best to avoid sheltered north to easterly slopes, where this layer is most likely to be a problem.