Reactive slabs will develop throughout the week as snow accumulates. Be prepared to back off if slopes are getting loaded by fresh snow or wind.
Avalanche Problem 1: Wind Slabs




- Be increasingly cautious as you transition into wind affected terrain.
- Avoid exposure to terrain traps where the consequences of a small avalanche could be serious.
Avalanche Problem 2: Persistent Slabs




Weak layers buried 60-80 cm below the surface may be reactive in thin snowpack areas or triggered with heavy loads such as a smaller avalanche.
- Back off if you encounter whumpfing, hollow sounds, or shooting cracks.
- Avoid convexities or areas with a thin or variable snowpack.
Avalanche Summary
Warm alpine temperatures over the weekend caused a natural cycle of large wet loose avalanches (up to size 2.5) on steep solar aspects throughout the region. Some smaller wind slab avalanches were reported in cross-loaded gullies around Bear Pass.
Snowpack Summary
Surface snow is well settled after a weekend of warm alpine temperatures. Wind slabs are lingering on a range of aspects after strong southerly winds on the weekend and outflow winds last week.
Below the most recent precipitation, up to 40 cm recent snow overlies several layers of interest in the upper snowpack. These include crusts, surface hoar and facets. A hard crust with associated facets from mid-December sits deeper in the snowpack, about 60 cm down. These layers have been reactive in recent snowpack tests and could potentially be triggered to release large avalanches.
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
TUESDAY: 5-15 cm of new snow, strong south winds, freezing level dropping to 700 m.
WEDNESDAY: More flurries with 10-20 cm of new snow, strong south winds, freezing level steady at 700 m.
THURSDAY: Another 10-20 cm of new snow, strong south winds, freezing level steady at 700 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.
Strong southerly winds have blown recent snow into fresh wind slabs in lee terrain. Older, more stubborn wind slabs from recent outflow winds may still be reactive around ridge crests and on cross-loaded features at lower elevations.