Avoid all slope with cornices overhead as there is recent evidence of them falling recently. This is considered a large trigger on the slope below.
Avalanche Problem 1: Wind Slabs




- Use caution in lee areas. Recent wind loading has created wind slabs.
- Use caution on open slopes and convex rolls
Avalanche Problem 2: Loose Wet




Pay close attention to the effect of solar radiation and daytime warming. Point release from rocks and cliff terrain can trigger isothermal snow below. This will be of most concern in the late afternoon.
- Avoid terrain traps, such as gullies, where the consequences of a small avalanche could be serious.
- Use extra caution on solar slopes or if the snow is moist or wet.
Avalanche Problem 3: Persistent Slabs




These events require a significant force to trigger them such as a large cornice failure or avalanche debris from above. Once triggered they can be very large and run far into the valley below. Many slopes have already been triggered.
- Pay attention to overhead hazards like cornices which could easily trigger deep slabs.
- Avoid shallow snowpack areas where triggering is more likely.
Avalanche Summary
No patrol Friday. In the past 48hrs persistent slab avalanches up to size 3.5 have occurred from alpine terrain. They are size 2-2.5 and are are being triggered by cornice failures or small windslab avalanches stepping down to these deeper layers. With freezing levels reaching treeline expect some loose avalanches on South to West facing slopes.
Snowpack Summary
Windslabs are up to 40cm deep. Sun or temperature crusts extend to treeline and continued into the alpine on southerly slopes. Persistent slabs can be found on most aspects at treeline and above. These have been most reactive recently to large triggers like cornice failures. Below 1,900m the snowpack is isothermal.
Weather Forecast
Saturday will be cloudy, sun and flurries, 5cm of snow, -2 C, West winds 25-50km/hr, and freezing level 1900m. Sunday will be a mix of sun and cloud, -10 to -5, West winds 15-45km/hr, and freezing level 1600m. Monday will be sun and cloud, no precipitation, -9 to plus 1 C, light winds, and 2400m freezing level.
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
- Avalanche Bulletin - Jasper National Park URL:
http://www.avalanche.ca/api/forecasts/jasper.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.
Although mostly thin some wind slabs are up to 40cm thick in alpine terrain. Solar radiation and cornice collapses can trigger these events. Once triggered the potential to trigger deeper weaknesses exists resulting in larger avalanches.