Regions
Northwest Coastal.
Variability exists within the region. Avalanches resulting from solar warming are possible with the intense March sunshine.
Confidence
Fair - Timing or intensity of solar radiation is uncertain
Weather Forecast
Flurries are expected Sunday, Monday is more likely to be dry. Sunny breaks for both days, freezing level around 500 m. Winds light to moderate southerly. Similar weather expected for Tuesday morning, although winds may ramp up from the south building for a frontal system expected to bring snow Tuesday afternoon.
Avalanche Summary
An avalanche cycle occurred on Friday in response to the new snow and wind. Mostly the activity was relatively small and contained within the top 30 cm of the storm snow. However, some larger events up to size 3 were noted. 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.
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. The mid-pack varies greatly depending on location. You may find up to three persistent weak layers. First, a surface hoar layer buried mid-March, now buried 60-80 cm deep, seems to be most prevalent in the mountains around Stewart. Second, a surface hoar layer buried early March, buried around 1 m, has been causing problems north of Terrace. Third, a weak layer comprising surface hoar or facets, buried early February, is now more than 1 m down. This has been causing issues particularly in the north around Ningensaw. However, recent reports indicate this layer is becoming difficult to trigger. Bear in mind that triggering any of these persistent weak layers would likely result in a very large avalanche. 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.