Regions
Northwest Coastal.
A weak layer of surface hoar that is now buried around a metre deep is creating a low likelihood, high consequence scenario. Continue to investigate this layer carefully.
Confidence
Moderate - Due to the number of field observations
Weather Forecast
Monday: Sunny / Light easterly winds / High of -13 C.Tuesday: Sunny / Light northeasterly winds / High of -13 C.Wednesday: Sunny / Light northeasterly winds / High of -12 C.
Avalanche Summary
On Sunday, there was a report of a size 2 natural avalanche west of Terrace. It was on a southwest aspect and it was estimated that it failed on the mid-November surface hoar layer around a metre deep. This layer may remain reactive to human triggers in isolated locations for weeks and requires continued investigation.
Snowpack Summary
Clear skies and strong outflow winds have created a variety of snow surfaces including scouring and hard wind slabs in exposed areas and up to 12 mm surface hoar formation in sheltered areas. Strong to extreme easterly winds over the past few days have created wind slabs on aspects you may not expect them. Wind slabs could be present on all aspects in exposed alpine, treeline, and even some below treeline locations. A layer of surface hoar which was buried around November 22nd is down 60-120 cm in many parts of the region. This layer is likely still reactive to human triggers. A thick rain crust exists 20-30 cm below the surface hoar layer, with isolated reports of weak facets (sugary snow) forming above the crust; however, that interface has not become a concern as of yet. Treeline snow depths are around 140-200 cm in the Terrace and Stewart areas, but substantially less further north. Concerns in the north are basal weaknesses that may exist in the shallower snowpack areas especially on smooth alpine features like glaciers.
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
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.