Avalanche Forecast
Issued: Mar 24th, 2014 9:45AM
The alpine rating is Storm Slabs, Persistent 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 Wednesday
Weather Forecast
Unsettled conditions are expected for Tuesday before a frontal system arrives Tuesday evening. Precipitation is expected for Tuesday night through to Wednesday night. Unsettled conditions are expected again for Thursday. Freezing levels are expected to be higher to the south of the region and precipitation amount are expected to be higher to the north of the region.Tuesday: Light scattered flurries possible 0-2cm, freezing level am: surface pm: 800-1400m, ridgetop wind: light SE-SWTues. Night/Wednesday: Snowfall 15-25cm, freezing level am: 300-700m pm: 600-1200m, ridgetop wind: light SWThursday: Scattered flurries 2-5cm, freezing level am: surface pm: 800-1400m, ridgetop wind: light variable
Avalanche Summary
Reports from Sunday include natural and human-triggered avalanche activity up to size 1.5 within the recent storm snow, typically down 20-35cm, and natural sluffing from steep features. Early reports from Monday include a natural size 2 loose wet avalanche in the Rogers Pass area and a large slab avalanche release in the N Columbia region.
Snowpack Summary
The upper snowpack may have various non-persistent weak layers within the recent storm snow. This includes small surface hoar in sheltered areas, thin sun crusts on solar aspects, rain crusts at lower elevations, and/or small facets. These layers are not widespread and are not expected to persist very long but they continue to produce small slab avalanches. Weak cornices and stubborn wind slabs may also be a concern in some areas.There are three persistent weak layers that remain a concern. The mid-March sun crust/surface hoar layer is down 50-80cm. Recent snowpack tests suggest that the reactivity of this layer is becoming more isolated but many areas still have the potential for human-triggering. The early-March crust/facet/surface hoar layer is down around 80-120cm. Human-triggering has become less likely but the layer still has the potential to produce large avalanches and we continue to see activity stepping down to this layer. The mid-February crust/facet/surface hoar layer is typically down at least 1.5m and direct triggering has become unlikely. However, large triggers like cornices or smaller avalanches can still trigger this layer and produce very large avalanches.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Persistent 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 25th, 2014 2:00PM