There is some uncertainty as to how much snow is expected for Tuesday. Danger ratings will increase if amounts received exceed 5-15 cm as forecasted.
Avalanche Problem 1: Storm Slabs




- Use conservative route selection, choose moderate angled and supported terrain with low consequence.
- Watch for whumpfing, hollow sounds, shooting cracks or recent avalanches.
- Be careful with wind loaded areas, especially near ridge crests and roll-overs.
Avalanche Problem 2: Persistent Slabs




A weak layer exists 100-140 cm below the surface. It may still be possible for humans to trigger persistent slab avalanches on this layer, or for a storm slab release to step down to this layer resulting in a very large avalanche.
- Caution around convexities or areas with a thin or variable snowpack.
- Avoid areas with overhead hazard, avalanches triggered higher up may travel long distances.
Avalanche Summary
Sunday north of Meziadin Junction a natural size 4 and a natural size 3.5 were observed on a southwest and northeast aspect at 1800-2000 m and are suspected to have failed on the mid-January layer.
On Saturday wind and storm slab avalanches failed naturally to size 2 on a variety of aspects in both alpine and treeline elevation bands. A natural size 3 persistent slab avalanche was observed on a steep north facing alpine feature with a crown up to 100 cm in depth, which suggests the mid-January interface was involved. A another very large avalanche (size 3.5) was reported from an unknown aspect/elevation.
Natural avalanche activity was observed on Friday morning, producing several 30 cm thick slabs in the latest snow. A large (size 3) storm slab avalanche was reported on a east aspect east of Terrace.
A few persistent slab avalanches released on Wednesday, most likely failing on the mid-January crust. This included a natural size 3 avalanche on a southwest slope at 1150 m near Exstew and a few skier triggered slabs (size 1-2) in thinner snowpack areas (east of Terrace and the northern part of the region).
Snowpack Summary
Another 15-25 cm of new snow since Sunday morning brings settled storm snow accumulations to 50-80 cm over the past week.
A weak layer buried in mid-January is 100-140 cm below the surface and remains a concern. In most areas this layer is a crust, but it may also be surface hoar in sheltered areas at treeline and below. This layer produced a few human triggered avalanches throughout the region over the past week, and may remain reactive as it adjusts to the weight of the new snow.
In thinner snowpack areas (north and inland), deeper crust / surface hoar layers that were buried in December and early January may still be a concern. They are buried over 150 cm below the surface, but may be triggerable from shallow spots.
Weather Forecast
TUESDAY: Cloudy, flurries. Accumulation 5-15 cm. Ridge wind moderate, southwest. Temperature -2. Freezing level 600 m.
WEDNESDAY: Snow. Accumulation 15-25 cm. Ridge wind light gusting to strong, west. Temperature +2. Freezing level 1700 m.
THURSDAY: Mix of sun and cloud. Ridge wind light, northeast. Temperature -1. Freezing level 800 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.
Significant snow and wind have formed storm slabs that have been reactive to both human and natural triggers at higher elevations and in wind-affected terrain. More snow and wind will continue to build these slabs.