Rising freezing levels, light rain, and the sun's influence are the main concerns for the next few days. Watch for moist or wet snow. Recent wind slabs may also become more sensitive to triggering with the warming trend.
Avalanche Problem 1: Loose Wet




- Use extra caution on slopes if the snow is moist or wet.
- Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.
Avalanche Problem 2: Wind Slabs




Strong to extreme winds have created widespread wind slabs in leeward areas in the alpine. With warming temperatures these slabs may still be sensitive to light triggers, such as a small slough or a skier/rider.
- Be careful with wind loaded areas, especially near ridge crests and roll-overs.
- Pay attention to overhead hazards like cornices which may become weak with warming.
Avalanche Summary
On Sunday there was a report from the Howson range of a natural, size 2 wind slab release on a wind-loaded, northeast aspect at 2050 m, as well as evidence of previous widespread smaller activity as a result of wind loading.
Last week, on Thursday a widespread natural avalanche cycle (up to size 2), triggered by intense wind loading was reported from the northern part of region.
While on Wednesday, a natural size 3.5 avalanche that initiated as a storm slab then stepped down to a deeper weak layer, and a solar triggered size 2 avalanche were reported from the Howson range. Skier triggered size 1 storm slab releases on a buried sun crust (30 cm deep) on a southeast aspect at 1700 m were also reported in the same area.
Snowpack Summary
Rising freezing levels and daytime warming have created moist or wet snow surfaces on all but alpine, northerly aspects where 20 cm up to 50 cm of recent storm snow has been redistributed by strong winds.
Weak layers buried around March 19th are roughly 40 cm below the surface (up to 100 cm in deeper snowpack areas). These weak layers include surface hoar on shaded aspects at high elevations and hard crust layers on solar aspects and below treeline.
Near the bottom of the snowpack, weak and sugary facets are found in shallow, rocky snowpack areas. Storm slabs have stepped down to these facets and producing very large avalanches in northern parts of the region.
Weather Forecast
TONIGHT: Mostly cloudy. Ridge wind moderate, south. Alpine temperature near 0. Freezing level 1600 m.
TUESDAY: Cloudy, wet flurries. Accumulation 5-10 cm. Ridge wind strong to extreme southeast. Alpine temperature near 0. Freezing level 1600 m.
WEDNESDAY: Mix of sun and cloud. Ridge wind moderate to strong, southeast. Alpine temperature near 0. Freezing level 1500 m. Snow beginning in the evening.
THURSDAY: Mix of sun and cloud, snow ending. Accumulation 5-10 cm. Ridge wind light, southwest. Alpine temperature near -2. Freezing level 1200 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
- Northwest Inland URL:
http://www.avalanche.ca/api/forecasts/northwest-inland.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.
Recent storm snow may become unstable due to rising freezing levels and wet snow or rain. Once moving a loose wet release may have the potential to trigger a slab on a deeper weak layer.