A stable weather pattern with little precipitation is expected in the next few days. Should the sun pop out, it could destabilize sun-exposed slopes and weaken cornices.
Wind slabs formed from Thursday's snow and strong south to southwest wind could still be triggered by riders. The most suspect terrain is immediately adjacent to ridges at treeline and alpine elevations. Note that cornices are large, looming, and could fail during periods of intense sun or from the weight of a human.
A weak layer of feathery surface hoar may be found around 40 to 80 cm deep on northerly aspects around treeline and lower alpine elevations. This layer may be spotty and only found in sheltered terrain features. The latest avalanche activity was in the north of the region on March 6. The layer has been dormant in the south (e.g. around Coquihalla), where snowpack tests are suggesting that the layer may be bonding. Assess the layer in the snowpack prior to committing to avalanche terrain or adopt a conservative mindset to avoid the problem.
In the north of the region (e.g. Duffey, Hurley, Goldbridge), a persistent weak layer of faceted grains near the ground presents a lingering concern on steep, shallow slopes in the alpine.
SUNDAY Night: Clear periods, light southwest wind, alpine temperature -8 C.
MONDAY: Clear skies, light west wind, alpine temperature -5 C, freezing level 1000 m.
TUESDAY: Cloudy with scattered flurries, moderate southwest wind, alpine temperature -4 C, freezing level 1200 m.
WEDNESDAY: Cloudy with scattered flurries, moderate to strong southwest wind, alpine temperature -5 C, freezing level 1100 m.
On Sunday there was skier triggered size 2 persistent slab avalanche in the north of the region that is suspected to have run on weak facets that were buried in late November. It was on a northwest aspect at 2200 m and may have been a slope that had slid previously and was reloaded.
On Friday, explosives triggered cornices and 20 cm slabs within the recent storm snow, producing small (size 1 to 1.5) up to large (size 2) avalanches. The avalanches were on west to north aspects and at alpine elevations. A persistent slab avalanche was triggered by a rider in the northern part of the region, likely releasing on the surface hoar layer described in the Snowpack Summary. The avalanche was large (size 2), in alpine terrain, and on a northerly aspect.
15 to 25 cm falling late last week with strong south to southwest wind has formed wind slabs in lee terrain features at treeline and alpine elevations.
A weak layer of surface hoar crystals and/or faceted grains may be found around 40 to 80 cm deep on northerly aspects at treeline and lower alpine elevations. The layer may have been destroyed by strong wind immediately before burial on February 22nd, but it may still exist in sheltered terrain features. Where it exists, it has been reactive in some snowpack tests but not others, suggesting spatial variation. This persistent weak layer warrants investigation and a conservative terrain use strategy. Check out the latest forecaster blog that offers a deeper dive into these conditions.
In the northern part of the region (i.e., Duffey/Hurley/Goldbridge), a deep instability may linger at the base of the snowpack. It has not produced an avalanche since February 17th. Human-triggering is unlikely, though if one were to trigger the layer, it would likely be in a thin, shallow, rocky spot. A large load, such as from a cornice fall, or rapidly changing weather have the potential to trigger this layer.
