Fresh storm slabs have formed over a weak and unstable snowpack. The continuing storm will keep the snowpack near a tipping point. Keep seeking out simple terrain that is free of overhead hazard.
Avalanche Problem 1: Storm Slabs




- Choose sheltered terrain where new snow hasn't been wind-affected.
- If triggered, storm slabs may step down to deeper layers and result in very large avalanches.
Avalanche Problem 2: Persistent Slabs




Several deeply buried weak layers are persisting in the snowpack and continue to produce very large avalanches - especially with heavy triggers. This is a time to carefully measure your exposure to avalanche terrain and to avoid overhead hazards.
- Seek out low angle, low consequence terrain as well as terrain that has seen heavy traffic.
- Either avoid or space out and travel quickly through runout zones of avalanche paths.
Avalanche Summary
On Saturday, a large persistent slab avalanche was remote triggered by a snowmobiler approaching a convex slope in the Allan Creek area. The crown fracture was over a metre deep. Two recent size 2.5 natural persistent slab avalanches that failed on the mid-December weak layer were observed at 1500-1700 metres in the Monashees just south of the region.
Explosive control work on Thursday produced avalanches to size 2.5 failing on both the mid and early January interfaces. These avalanches ran on north, northeast, east and southeast facing features between 1600 and 2600 m.
Reports from Wednesday showed numerous recent size 2-3 releases on all aspects at all elevations, with several avalanches that reached size 4. Subsequent explosives control yielded storm slab and wind slab releases from size 2-2.5 and persistent slab results generally from size 2.5-3. The early January persistent weak layer was named as the primary failure plane for persistent slab releases, although several larger releases stepped down to the mid-December layer.
On Tuesday, a size 2.5 avalanche on a northeast facing slope at 1920 m resulted in a single fatality in Clemina Creek. More details available here.
Snowpack Summary
15-25 cm of new snow fell over the region over Thursday night and Friday, bringing recent storm snow totals to 40-80 cm. This snow sits on an unstable snowpack with three active weak layers we are monitoring:
1) The first layer is found beneath the recent storm snow and is formed of a crust and/or surface hoar layer that was buried in mid-January. The surface hoar is up to 10 mm in size, found at all elevation bands and has been very reactive on north through east aspects between 1900-2600 m.
2) Deeper in the snowpack, the early-January persistent weak layer is found 60 to 120 cm below the surface. This layer has been reported as the most active persistent weak layer during a recent natural avalanche cycle that took place in the region. It has also been the most reactive to recent explosives control.
3) Another weak layer buried mid-December consisting of a facet/surface hoar/crust combination is buried 110 to 160 cm deep. It has been most problematic at and below tree line. Many avalanches that failed at shallower weak layers 'stepped down' to this interface during the recent avalanche cycle and in recent explosives control.
Weather Forecast
Sunday: Mainly cloudy with scattered flurries bringing approximately 5 cm of new snow. Light variable winds. Alpine high temperatures around -10.
Monday: A mix of sun and cloud. Light west winds. Alpine high temperatures of -11.
Tuesday: Cloudy with flurries bringing 5-10 cm of new snow, increasing overnight. Light to moderate west winds. Alpine high temperatures of -5.
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
- Cariboos URL:
http://www.avalanche.ca/api/forecasts/cariboos.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.
Friday's storm formed new storm slabs at all elevations and ongoing snowfall will continue to build and add mass to these slabs. The problem is especially concerning at alpine elevations where strong winds have made slabs extra thick and reactive.