Avalanche Forecast
Issued: Mar 9th, 2017 5:37PM
The alpine rating is Storm Slabs, Cornices and Deep Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Moderate - Timing or intensity of solar radiation is uncertain on Saturday
Weather Forecast
Thursday night: 10-15cm of new snow / Moderate southwest winds / Alpine temperature of -8Friday: 12-18cm of new snow / Strong to extreme southwest winds / Alpine temperatures of -3 (freezing levels at 1500m)Saturday: Clear skies in the morning with increased cloud in the afternoon / Light southwest winds / Alpine temperature of -3Sunday: Light flurries / Light southwest winds / Alpine temperature of -4
Avalanche Summary
Over the past few days, natural and human-triggered storm slab and loose dry avalanches to size 2 were reported on a variety of aspects. Cornices are large and remain easy to trigger. A great image from Sunday illustrates just how surprising the results can be. Click here for details. A size 3.5 deep persistent slab avalanche also occurred on a northeast facing alpine slope on Mt Hosmer. The avalanche, which likely occurred on Wednesday, is thought to have been cornice-triggered and ran a distance of about 900m. This event highlights the isolated, yet destructive, nature of the deep persistent avalanche problem which should become more prevalent as we head into spring.Looking forward, natural storm slab activity is expected to ramp-up again in response to new snow and wind on Thursday night and Friday.
Snowpack Summary
By Friday morning expect 10-15cm of new snow with lots more falling throughout the day. Strong southwest winds are expected to shift these accumulations into much deeper deposits in exposed lee terrain. The overall storm total for the last week or so now stands at roughly 80-130 cm. At times, strong southwest winds have extensively redistributed the snow forming large brittle cornices. In some areas the recent storm snow is settling into a cohesive slab which sits over a variety of old surfaces including surface hoar, facets, stiff wind slabs, sun crusts, and a rain crust below 1900 m. Little is known about the reactivity of this interface which was buried in the middle of February. Until we get a better feel for it, I'd assume it has potential for large and destructive avalanches.Isolated basal facets still exist in shallow snowpack areas and can produce destructive full-depth avalanches. Likely triggers include intense storm loading, a cornice fall, or strong solar radiation.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Cornices
Aspects: North, North East, East, South East, South.
Elevations: Alpine.
Likelihood
Expected Size
Deep Persistent Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Valid until: Mar 10th, 2017 2:00PM