New snow and wind will load several buried weak layers in the snowpack. Choose conservative terrain and minimize exposure to overhead hazard. Large avalanches may run long distances.
Avalanche Problem 1: Storm Slabs




- Avoid lee and cross-loaded terrain near ridge crests or convex rolls.
- Watch for whumpfing, hollow sounds, shooting cracks or recent avalanches.
Avalanche Problem 2: Persistent Slabs




There is limited information about weak layers buried 60-100 cm below the surface. They produced a few large avalanches last week, and may remain sensitive to human triggering in shallow snowpack areas.
- Avoid lingering in runout zones, avalanches triggered up high may run long distances.
- Avoid shallow or thick to thin snowpack areas where triggering a deeper layer is more likely.
Avalanche Summary
On Monday evidence of a natural avalanche cycle from size 1.5-2.5 was reported on north through south aspects between 1200-1600 m in the Howson Range failing both in the recent storm snow as well as the deeper mid-December layer. A natural size 2.5 that failed on a deep weak layer of sugary, facets at the base of the snowpack was also reported from the northern part of the region near Ningunsaw.
On Saturday a small storm slab was reportedly human triggered on an east facing aspect around 1000 m. And at the start of the storm on Wednesday and Thursday skiers triggered a few small slabs on steep convex rolls.
Last week some large (size 2-3) natural persistent slab avalanches in the Howsons, and two large (size 2.5) remotely triggered avalanches north of Kispiox were reported. We have no information from the Smithers area, but suspect a similar deeper weakness could exist there too. Activity on buried weak layers is most suspect during periods of heavy loading or rapid warming, hence it's time to be cautious.
Snowpack Summary
Approximately 30-50 cm of storm snow has accumulated since last Thursday. The snow has mostly fallen as low density powder, but may have settled in some areas that experience a brief period of warming on Friday.
A crust and/or weak feathery surface hoar layer buried in mid-January now lies 60-100 cm below the surface. The crust exists well into the alpine and the surface hoar can be found in sheltered areas in the lower alpine and treeline elevations.
Another two crust / surface hoar layers that were buried in December are now 80-120 cm below the surface. These layers produced sudden results in recent snowpack tests and have been the suspected weak layer in recent large remotely (from a distance) triggered avalanches.
Weather Forecast
TONIGHT: Cloudy, flurries. Accumulation 5-10 cm. Ridge wind moderate, west. Temperature -4. Freezing level valley bottom.
WEDNESDAY: Snow. Accumulation 10-15 cm. Ridge wind light to moderate, southwest. Temperature -6. Freezing level valley bottom.
THURSDAY: Mostly cloudy, light flurries. Accumulation trace. Ridge wind light, northeast. Temperature -12. Freezing level valley bottom.
FRIDAY: Sunny. Ridge wind light, northeast. Temperature -12. Freezing level valley bottom.
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 Inland URL:
http://www.avalanche.ca/api/forecasts/northwest-inland.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.
New snow and wind will form new storm slabs particularly at upper elevations and in wind-exposed areas. These slabs may be reactive to human triggering and a release may have the potential to step-down to a deeper layer buried in the snowpack.