Avalanche Forecast
Issued: Mar 23rd, 2014 9:09AM
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
A weak ridge of high pressure will be the main feature for Monday. Unsettled conditions are expected for Monday night and Tuesday before the next frontal system arrives Tuesday afternoon or evening. Precipitation is expected for Wednesday and Thursday. Monday: A mix of sun and cloud, freezing level am: surface pm: 1200m, ridgetop wind: light variableMonday Night: Scattered flurries 1-3cmTuesday: Mostly cloudy, freezing level am: 500m pm: 1500-1800m, ridgetop wind: light S-SWTues. Night/Wednesday: Snowfall 15-25cm, freezing level am: 500-1000m pm: 1400m, ridgetop wind: light SW-W
Avalanche Summary
We are still seeing relatively small inputs, like periods of strong winds or brief sunny breaks, trigger persistent slab avalanches. Many of these events have occurred on southerly aspects from slopes in the alpine or at treeline. Extra caution is advised when the sun is out.On Saturday, we received reports of isolated skier-triggered storm slab avalanches up to size 1.5 in the upper 20cm. Early reports from Sunday suggest increased natural and human-triggered avalanche activity up to size 1.5 within the recent storm snow, typically down 20-35cm.
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 24th, 2014 2:00PM