South Rockies Avalanche Forecast
Mar 20th, 2020 4:00PM
Clouds may temper day-time warming. Minimize exposure to cornices and steep slopes that face the sun during the warmest part of the day. A deep weak layer remain a concern.
Friday night: Clear. Moderate northwest wind. Freezing level valley bottom.
Saturday: Mix of sun and cloud with flurries in the evening bringing 5-10 cm. Light northwest wind. Freezing level 1900 m.
Sunday: Mix of sun and cloud. Moderate southwest wind. Freezing level 1700 m.
Monday: Scattered flurries. Strong southwest wind. Freezing level 1800 m.
A single snowmobile triggered size 1 wind slab was observed amid extensive slope "testing" on Friday. In neighboring Waterton National Park, solar-triggered loose dry and wind slabs up to size 1.5 were observed Thursday, having run surprisingly far on a crust. A size 2 deep persistent slab out of steep, thin, rocky alpine terrain reminds us that the basal facets still exist and can be triggered in this type of terrain.
If you decide to travel in the backcountry, consider sharing your observations with us and fellow recreationists via the Mountain Information Network (MIN) to supplement our data stream as operators are shutting down. Even just a photo of what the day looked like would be helpful.
Sunny skies have formed a melt-freeze crust on sun-exposed slopes. The alpine consists of wind affected snow from easterly wind, so you may find small pockets of wind slabs in atypical terrain features on south to west aspects.
A layer of faceted grains overly a melt-freeze crust from early February. This layer currently sits 40 to 80 cm below the surface.
The base of the snowpack contains basal facets that are most prominent in shallow, rocky start zones.
Terrain and Travel
- Carefully evaluate steep lines for wind slabs.
- Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.
- Rocks will heat up with daytime warming and may become trigger points for loose wet avalanches
- Be aware of the potential for large avalanches due to the presence of a deep persistent slab.
Modest air temperature and sunny skies combine to weaken the snow surface. As this occurs, loose wet avalanche activity may result. The highest likelihood of this occurring is during the heat of the day on sun-exposed slopes. Note that the same warming trend also weakens cornices, so best to stay well back from them on ridges and avoid travelling beneath them.
Aspects:East, South East, South, South West, West.
Deep Persistent Slabs
Weak snow at the bottom of the snowpack hasn't gone away. Evidence of deep persistent slab avalanches has been focused in the Sparwood-Elkford area over the past month. Human triggering is most likely around steep, rocky terrain features or anywhere the snowpack is thin and weak. A failing cornice could initiate a deep persistent slab when it impacts the slope below.
Valid until: Mar 21st, 2020 5:00PM