Regions
Northwest Coastal.
Weather Forecast
Generally settled weather with flurries possible throughout the forecast period, Saturday, Sunday and Monday. Winds generally light, initially from the southeast, becoming southerly on Sunday and Monday. Freezing levels going up to around 800 m during the day and dropping down to valley bottom each night.
Avalanche Summary
On Thursday, two natural slab avalanches were observed, one size 1.5 on a north aspect at 1250 m with a fracture line 40cm deep in the recent storm snow. The other was a glide release at 575m near Terrace caused by warm temperatures. Numerous wet loose avalanches were also observed. On Wednesday, a size 3 natural cornice failure was observed in the region on Wednesday.
Snowpack Summary
Sporadic strong and variable winds have redistributed moderate amounts of recent storm snow into wind slabs that most commonly exist in the lee of terrain features 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.