Freezing levels above the mountain tops and sunny skies are warming the snowpack, particularly around midday. Best to avoid sunny slopes and overhead avalanche terrain. Read our blog on the impact of warming.
Avalanche Problem 1: Deep Persistent Slabs




- Pay attention to overhead hazards like cornices which could trigger deep persistent slabs.
- Avoid steep, rocky, and shallow snowpack areas where triggering deeper layers is more likely.
- Steep, south facing slopes are the most likely areas to trigger deeper layers.
Avalanche Problem 2: Loose Wet




High freezing levels and sunny skies are causing intense warming of the snowpack on solar aspects. Peak danger will likely be during afternoon hours. Pay close attention to the effects of the sun on avalanche terrain and avoid overhead exposure.
- Start early to stay off south facing slopes during the heat of the day.
- Watch for signs that the snow is heating up such as pin-wheeling and point-releases below cliffs.
- Avoid terrain traps such as gullies and cliffs where small avalanches can have high consequence.
Avalanche Summary
Loose wet avalanches were noted on solar aspects to size 1.5 on Sunday. Some of these triggered small slabs, about 10 cm deep.
The forecast warming and sunshine may wake up a deeper weak layer on steep south facing slopes resulting in large and destructive avalanches.
Snowpack Summary
Warm air temperatures and daytime sun have produced moist snow on solar aspects into the alpine and moist snow on all aspects up to around 1400 m. On shady aspects at higher elevations, expect to find wind slabs in lee features and loose dry in sheltered features.
Cornices are large and prone to failure with warm air temperatures and sunny skies.
The upper/mid-pack is generally well-settled and strong. The lower snowpack is weak with a combination of crusts and facets near the bottom of the snowpack that are widespread. The primary concern is the potential of these deeper persistent weak layers becoming active by rapid warming of the snowpack through rising freezing levels and intense solar radiation. This is most likely to occur on south-facing slopes.
Weather Forecast
TUESDAY: Sunny, light southwesterly winds, alpine temperature 3 C, freezing level 3100 m.
WEDNESDAY: Mix of sun and cloud, light southwesterly winds, alpine temperature 3 C, freezing level 2500 m.
THURSDAY: Mostly cloudy with light snowfall, accumulation 2 to 5 cm, light westerly winds, alpine temperature -2 C, freezing level 1500 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
- South Rockies URL:
http://www.avalanche.ca/api/forecasts/south-rockies.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.
Deeply buried weak layers linger near the base of the snowpack. These layers are most likely to be triggered from thin snowpack areas. Avoid lingering below corniced ridges, as a cornice fall could trigger deeper layers.