Avalanche Forecast
Issued: Mar 18th, 2017 3:47PM
The alpine rating is Storm Slabs and Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Moderate - Intensity of incoming weather systems is uncertain
Weather Forecast
We'll see lingering flurries on Sunday as it cools down significantly. Clearing Monday onwards.SUNDAY: Cloudy with isolated flurries / moderate to strong west wind / Alpine temperature -8 / Freezing level 800mMONDAY: Increasing cloud in the afternoon and some scattered flurries / Light east wind / Alpine temperature -6 / Freezing level 1100mTUESDAY: Isolated flurries (5cm possible)Â / Light southerly wind / Freezing level 1500m
Avalanche Summary
The past several days have seen widespread natural avalanche activity at all elevations and on all aspects, including a Size 4.5 in the central Selkirk range reported Thursday (crown height up to 3.5 m high, running 1200 vertical metres and leaving debris up to 28 metres deep) and a Size 3.5 near the Valhallas on a southeast aspect near 2400m.Many of these avalanches ran in the storm snow with some also stepping down to persistent weaknesses (see snowpack summary below) deeper in the snowpack. Widespread wet slabs and loose wet avalanches have also been reported below treeline.
Snowpack Summary
Heavy wet snow (15-20 cm in 12 hours) and moderate southerly winds started late Friday and continued through Saturday. Temperatures also warmed up significantly. The end result: Widespread storm slabs and wind slabs at treeline and above with significant cornice growth as well. All this storm snow (totals of 40-80cm) sits on older windslabs (or soft slabs) at treeline and above. Below 1800m, the new snow sits on a melt-freeze crust from last week's warm storm, and reports so far are that the new snow is bonding well to the old crust. Approximately 100-140 cm below the surface you may find the late-February persistent weakness / crust interface. This layer has woken up from time to time as smaller avalanches still have to potential to 'step down' and trigger this layer. The deep mid-December facet layer (and November raincrust) still linger at the bottom of the snowpack and are the suspected culprit (running to ground) in a Glacier National Park avalanche. See here for the spooky picture.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Mar 19th, 2017 2:00PM