New snow (possibly 20 cm by Sunday) and wind will continue to build slabs and cornices at upper elevations. Sloughing, and cracking around skis and sleds are signs that the new snow is bonding poorly to the old surface.
Avalanche Problem 1: Wind Slabs




- If triggered the wind slabs may step down to deeper layers resulting in large avalanches.
- Watch for whumpfing, hollow sounds, and shooting cracks.
- Be careful with wind loaded pockets, especially near ridge crests and roll-overs.
Avalanche Problem 2: Persistent Slabs




Buried weak layers exist in the snowpack and may be reactive to large triggers such as a cornice or step-down from a wind slab release. Human triggering may also be possible from shallow or thin. rocky, unsupported terrain.
- Pay attention to overhead hazards like cornices which could easily trigger the deep persistent slab.
- Avoid steep convexities or areas with a thin or variable snowpack.
Avalanche Summary
Tuesday through Thursday there have been numerous reports of skier triggered slab avalanches up to size 2 on predominantly steep, southeast to southwest-facing features between 1900-2000 m, that failed on the mid-February crust. As well as explosive control results up to size 2 and a remotely triggered (from a distance) pocket of hard wind slab near ridge top.
On Monday, natural wind slab avalanches to size 2.5 were reported on a southwest through northwest aspects between 1800m and 2400m.
Last weekend (Feb 17 & 18) we there were reports of widespread natural wind slab activity above 1900m on primarily south east through west aspects, as well as a wind slab release stepping down to deeper weak layers and triggering a size 3.5 persistent slab, on a south west aspect near 2300m.
Although deeper, persistent avalanche activity has become less frequent over the past week, light triggers in shallow rocky areas, as well as large triggers such as a cornice collapse or step down from a wind slab release, still have the potential to result in large destructive avalanches.
Snowpack Summary
A light dusting of new snow on Friday now covers 40-60 cm of storm snow from last week that has settled into a slab and been redistributed with previously strong winds into stiff wind slabs in wind-exposed areas.
These accumulations sit on an interface the was buried mid-February consisting of; a mix of older wind slabs in exposed higher elevation terrain, a sun crust on steep solar aspects, a rain crust below 1600m, and surface hoar on sheltered slopes.
Below the snow surface, several persistent weak layers make up a complex snowpack which is slowly beginning to show signs of improving. In the top 150-200 cm of the snowpack, two surface hoar layers buried in January can be found. Expect to find one or other of these on all aspects and elevations.
Deeper in the snowpack (200-250 cm) is a facet/crust/surface hoar layer from December that is most prevalent at treeline and below.
Near the base of the snowpack is a crust/facet combo from late November.
Weather Forecast
TONIGHT: Flurries. Accumulation up to 5 cm. Ridge wind light, southwest. Temperature -16. Freezing level valley bottom.
SATURDAY: Cloudy, light flurries increasing overnight. Accumulation 5 cm. Ridge wind light, southwest. Temperature -10. Freezing level valley bottom.
SUNDAY: Snow. Accumulation 10-15 cm. Ridge wind moderate to strong, west. Temperature -8. Freezing level 500 m.
MONDAY: Cloudy, light flurries. Accumulation trace. Ridge wind light, west. Temperature -8. Freezing level 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
- North Columbia URL:
http://www.avalanche.ca/api/forecasts/north-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.
New snow and wind are adding to reactive wind slabs that exist in many areas the alpine as well as open areas at, or near treeline. Previous strong winds have also formed large, fragile cornices at ridge tops.