Regions
Northwest Coastal.
Confidence
Fair - Intensity of incoming weather is uncertain on Thursday
Weather Forecast
Friday: Light snowfall - light southerly winds - freezing level at 600m Saturday: very light snowfall with a chance of intermittent sun - light and variable winds - freezing level at 300m Sunday: scattered cloud - light westerly winds - freezing level at 200m
Avalanche Summary
A size 3 natural cornice failure was observed in the region on Wednesday. Recent heli bombing in the northern part of the region produced mostly thin soft slab avalanches to size 2 that formed due to recent wind loading. With continued wind and snow throughout Thursday, I expect continued wind slab avalanche activity in the alpine and at treeline.
Snowpack Summary
Sporadic strong and variable winds have redistributed light amounts of recent storm snow into thin wind slabs that most commonly exist at treeline and in the alpine.In the northern part of the region two persistent weak layers are on the radar of some operators: Surface hoar buried at the beginning of March is as much as 70cm deep. The early February persistent weak layers (surface hoar, facets, crusts) are over a metre down. Although triggering persistent weaknesses has become less likely, persistent slabs would be destructive in nature, particularly below treeline on isolated and sheltered steep terrain where buried surface hoar may be preserved. Cornices in the region are reported to be very large and potentially unstable.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.