Fresh shallow wind slabs and sluffing should be manageable Saturday, but we can't forget about the potential for large human triggered persistent slab avalanches that seem to be most reactive on south facing terrain at upper elevation.
Avalanche Problem 1: Persistent Slabs




- Minimize exposure to steep south-facing slopes where recent storm snow overlies a crust.
- Use caution around sheltered steep or convex slopes where buried surface hoar may be preserved.
- Pay attention to overhead hazards like cornices which could trigger persistent slab avalanches.
Avalanche Problem 2: Storm Slabs




5 to 15 cm of new snow is expected Saturday accompanied by southerly wind. Watch for changing conditions, widespread sluffing and the formation of fresh shallow slabs which will likely be most problematic immediately lee of ridge crest.
- Be especially careful with wind loaded pockets near ridge crests and roll-overs.
- Saturday's storm snow will hide stubborn old wind slabs that may remain sensitive to triggering.
- Be cautious of sluffing in steep terrain.
Avalanche Summary
On Thursday warming temperatures initiated large loose wet avalanches to size 3 on south facing aspects between 2100 and 2700 m in the neighboring Glacier National Park. A natural size 2.5 wet slab was observed on a southeast facing feature at 2200 m as well.
On Tuesday a skier accidently triggered a size 1.5 persistent slab avalanche on an east facing slope at 2200 m with a crown 50 cm in depth. Two more avalanches to size 2 were remote triggered on a south/southeast facing slope between 2050 and 2150 m, likely running on the mid-March interface. A cornice fall on a southeast facing feature around 2500 m produced a size 3 persistent slab that likely ran the night of April 1st.
Snowpack Summary
Warming temperatures and time have helped to settle the upper 30 to 40 cm of ageing storm snow and have formed a weak surface crust on all aspects aside from true north below 2000 m. Above 2000 m, temperatures have remained cold and the snowpack is still quite "winter-like."
The main concern is the mid-March Persistent Weak Layer (PWL) which is now 60 to 100 cm below the surface. This layer is composed of a crust on all aspects at low elevations. At upper elevations the layer presents as a crust on solar aspects (those that face south and west) and buried surface hoar on polar aspects (those that face north and east). The reactivity of this interface has been steadily decreasing, but it continues to produce large avalanches and the potential for deep 'step down' avalanches cannot be dismissed. Solar aspects are expected to be the most suspect as the freezing level begins to rise over the next few days.
Deeper persistent weak layers from January and December are still being reported by professional observers, but are generally considered dormant.
Weather Forecast
The struggle between "spring-like" and "Arctic-like" will continue for a few more days. Saturday's storm should deliver a good shot of snow with the highest amounts concentrated in the southern portion of the region. A more spring-like pattern begins to take shape on Sunday with freezing levels creeping towards 2000 m by Monday.
SATURDAY: Overcast, freezing level beginning near valley bottom rising to around 1500 m, light to moderate south/southwest wind, 5 to 15 cm of snow possible.
SUNDAY: Broken cloud cover, freezing level beginning around 500 m rising to about 1800 m, light to moderate westerly wind, 1 to 3 cm of snow possible.
MONDAY: Scattered cloud cover, freezing level beginning around 1500 m rising to about 2000 m, light to moderate westerly wind, trace of snow possible.
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
- South Columbia URL:
http://www.avalanche.ca/api/forecasts/south-columbia.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.
Weak crust and surface hoar 60 to 100 cm below the surface has shown prolonged reactivity since the last storm. South facing features have been the most reactive as of late, and this trend is expected to continue as temperatures rise next week.