A strong winter storm system is expected Monday night into Tuesday. Significant snow is expected, however amounts are uncertain. If snowfall amounts exceed forecasted values, avalanche hazard will increase.
Avalanche Problem 1: Storm Slabs




- Avoid freshly wind loaded features and leeward slopes.
- Whumpfing, shooting cracks and recent avalanches are all strong indicators of unstable snowpack.
- Give cornices a wide berth when travelling on or below ridges.
Avalanche Summary
On Sunday there was a report of a skier-triggered cornice failure (size 2) on a northwest aspect at 2100 m, as well as skier and sledder triggered storm slabs (size 1.5) on east and north aspects in the alpine. Explosive control work also produced cornice failures, size 2-3 with little effect on the slopes below.
Saturday we received reports of a natural avalanche cycle from size 2-3 that occurred during the storm in wind loaded and cross-loaded alpine terrain, as well as numerous reports of large (size 2) skier and sled triggered storm slabs including several size 1-2.5's remotely triggered from a distance. These avalanches are suspected to have failed on the recently buried (March 21st) surface hoar/crust layer. Read details of a personal account here.
On Friday explosive control work and ski cutting produced numerous storm slab results from size 1.5-2, as well as size 2 cornice results and few remote/sympathetically triggered size 1.5 releases. Crown depths generally ranged from 20-40 cm deep, although up to 60 cm in loaded alpine areas.
There was also a report of a skier triggered size 1.5 on Friday that surprised a group on a convex feature at treeline. Read MIN report
Snowpack Summary
Another 5-10 cm of storm snow with strong southerly wind Sunday night adds to last week's storm which delivered 20 to 50 cm of snow accompanied by strong to extreme wind out of the southwest, south and southeast. This storm snow rests on the March 21st interface, a mix of moist grains at low elevations, crusts on solar aspects at all elevations and surface hoar/facets on north/east facing features at treeline and alpine elevations. Some west facing features may have surface hoar on top of a crust.
Deeper in the snowpack, 80 to 140 cm below the surface is a combination of facets, surface hoar, and/or crust known as the mid-February layer. This interface has not been active recently, but it does continue to produce resistant planar results in snowpack tests.
The mid and lower snowpack are strong and well settled.
Weather Forecast
Forecasted snowfall amounts are uncertain for Monday night & Tuesday. Higher amounts are expected for areas near Squamish.
TONIGHT: Snow. Accumulation 10-20 cm. Ridge wind strong to extreme, southwest. Alpine temperature near -4. Freezing level 1500 m.
TUESDAY: Cloudy, flurries. Accumulation 5-10 cm. Ridge wind strong to extreme, west. Alpine temperature near -3. Freezing level 1600 m.
WEDNESDAY: Mix of sun and cloud. Ridge wind moderate, northwest. Alpine temperature near -5. Freezing level 1400 m.
THURSDAY: Cloudy, flurries. Accumulation about 5 cm. Ridge wind moderate, west. Alpine temperature near -5. 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
- Sea To Sky URL:
http://www.avalanche.ca/api/forecasts/sea-to-sky.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.
New snow and strong winds will form storm slabs at all elevations. This adds to recent storm snow which sits above a weak layer consisting of crusts, surface hoar and facets that has been most reactive at treeline and above.