Avalanche Forecast
Issued: Mar 13th, 2014 10:04AM
The alpine rating is Storm Slabs and Deep Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Fair - Timing, track, or intensity of incoming weather system is uncertain on Saturday
Weather Forecast
Synopsis: A quick hitting system passes over the region Friday before a significant and warm rain/snow event arrives Saturday night and then settles in Sunday. Precip amounts and freezing Levels vary significantly from one model to the next, thus overall confidence in this Wx is Fair. Friday: Freezing Level: 1000m - 1500m; Precip: 2/8mm - 2/10cm; Treeline Wind: Light, SW | Mod W at ridgetop.Saturday: Freezing Level: 1100m - 1600m; Precip: Nil; Wind: Mod, SWSaturday Night: Freezing Level: 1000m - 1600m; Precip: 4/16mm - 4/20cm; Treeline Wind: Strong, W | Extreme SW at ridgetop.Sunday: Freezing Level: 1000m - 1600m; Precip: 1/5mm - Trace/5cm; Treeline Wind: Mod, W | Extreme SW at ridgetop.
Avalanche Summary
Riders remote triggered avalanches to size 2 on steep NE facing slopes at treeline Wednesday. One natural size 3 on a relatively steep NE facing bowl feature was also observed, likely failing on the February 10th PWL.The group involved in a very close call with a size 3.5 avalanche in the Ozalenka Valley south of McBride submitted a great incident report. Check it out here.
Snowpack Summary
Up to 80 cm of recent storm snow rests on small grained surface hoar in sheltered areas and a sun crust on solar aspects. In upper elevation wind exposed terrain the new snow has been pushed into deep wind slabs by moderate SW winds.The freezing levels remain high (aprox. 1800m) in this spring like pattern. Below treeline the snowpack is seeing a daily melt freeze cycle that has left many features wet and sloppy by the afternoon. This has created an isolated wet slab problem that has been responsible for serious incidents recently. At ridgetop cornices are large and unsupported.The February 10th surface hoar/facet/crust combo is around a meter below the snow surface and widespread throughout the region. Surface avalanches in motion, cornice fall and/or solar radiation all have the potential to initiate an avalanche on this deeply buried weak layer. Interestingly, we continue to hear about remote triggering at this interface. For the most part, the mid and lower snowpack are strong and well consolidated.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Deep Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Mar 14th, 2014 2:00PM