Heads up! Large avalanches have the potential to reach run-out zones. Be aware what, or who, may be above you.
Special Avalanche Warning in effect for the interior ranges. Copy this address to view details: http://bit.ly/2nSOUyX
Avalanche Problem 1: Wind Slabs




- Use conservative route selection, choose moderate angled and supported terrain with low consequence.
- If triggered the wind slabs may step down to deeper layers resulting in large avalanches.
- Be cautious as you transition into wind affected terrain.
Avalanche Problem 2: Persistent Slabs




The snowpack is complex and continues to produce very large avalanches on weak layers now deeply buried below the surface.
- Be mindful that deep instabilities are still present and have produced recent large avalanches.
- Avoid shallow snowpack areas where triggering a deep layer is more likely.
- Avoid exposure to overhead avalanche terrain, large avalanches may reach the end of run out zones.
Avalanche Summary
There are no confirmed reports of avalanches from Friday, however is SAR responding in an incident involving a snowmobiler in the southern Slocan Valley that appears to be avalanche related.
On Thursday, several large and destructive natural slab avalanches occurred through the region up to size 2.5 on all aspects and elevations. Avalanche control using explosives triggered numerous loose wet avalanches up to size 2 and a significant size 3 storm slab avalanche. These were reported from SE-SW slopes above 1900 m.
Earlier in the week, two very large destructive avalanches up to size 3.5 were triggered remotely (from a distance) with crown depths up to 200 cm. At least one of these avalanches ran full-path, destroying mature trees.
Natural avalanche activity will likely taper off through the weekend with colder temps; however, slopes will remain primed for human triggers.
Snowpack Summary
Storm snow accumulations from the past week vary from 10-45cm across the region at upper elevations. In the alpine this new snow has been redistributed to leeward slopes from strong northwest winds. Below 1800 m, up to 5 cm of low density snow covers a thin crust.
This now brings 1- 2 m of settled snow sitting on three significant surface hoar/ crust layers that were formed early to mid-January, and back in December. Near the base of the snowpack a crust/ facet interface exists and will likely haunt us all season. These persistent weak layers that lurk within the snowpack are reactive, producing large and destructive avalanches.
The snowpack is extremely complex and requires respect and diligence at this time.
Weather Forecast
SUNDAY: Mix of sun and cloud. Ridge wind light to moderate, east. Temperature -10. Freezing level valley bottom.
MONDAY: Mostly sunny. Ridge wind light, north. Temperature -8. Freezing level valley bottom.
TUESDAY: Cloudy, light flurries. Accumulation trace. Ridge wind light to moderate, southwest. Temperature -8. Freezing level 800 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
- Kootenay Boundary URL:
http://www.avalanche.ca/api/forecasts/kootenay-boundary.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.
Storm slabs are reactive. Natural avalanche activity may taper off, but slopes are primed for human triggers. Be aware that a slab or loose snow release near the surface could also step down to deeper layers in the snowpack.