Pay close attention to how the new snow is bonding to the old snow surfaces, especially where it sits on surface hoar and buried crusts.
Avalanche Problem 1: Storm Slabs




- Use caution in lee areas in the alpine and tree line, especially south / west facing slopes.
- Observe for signs of instability, such as cracking, whumpfing, and avalanche activity.
Avalanche Problem 2: Loose Wet




If the sun comes out on Wednesday, expect the new snow to become reactive and/or slide naturally, especially from steep solar aspects.
- Watch for signs that the snow is moistening such as pin-wheeling and point-releases below cliffs.
- Be cautious of sluffing in steep terrain, particularly where the debris flows into terrain traps.
- Avoid exposure to sunny slopes
Avalanche Summary
On Tuesday, one size 1 wind slab was reported, entraining moist snow during warming. A few natural loose dry avalanches up to size 1.5 occurred on Monday.
Snowpack Summary
Up to 25 cm of low density snow fell Sunday overnight into Monday, combined with last weeks snow, this brings the total amount 30-40 cm. This new snow sits on a wide variety of old surfaces: a melt-freeze crust on sunny aspects, isolated old wind slab in the alpine near ridge crests and predominantly dry snow or surface hoar (up to 20mm in size) on north aspects above 1500-1800m.
A weak layer of surface hoar buried mid-February exists in parts of the region around 50 to 80 cm deep. The lower snowpack is weak with a combination of crusts and facets near the bottom of the snowpack that are widespread.
Weather Forecast
Wednesday: Mix of sun and cloud. Alpine temperatures near -2 and freezing levels near 1900m. Ridgetop winds light from the South.
Thursday: Snow amounts 5-10 cm, accompanied by strong ridgetop winds from the southeast. Freezing levels near 1700 m.
Friday: Cloudy with isolated flurries. Alpine high of -11 and freezing levels near 1500 m. Light to strong gusty southwest winds.
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.
Watch for signs of poor bonding of the new snow with underlying surfaces, especially the March 18th crust, which can be found almost everywhere except high north facing aspects. Dry loose sluffs may run fast and far on slippery crusts.