The snowpack is complex and quite variable right now. Buried weak layers remain reactive and conservative terrain selection remains critical. Extra caution is required during the heat of the day, especially on sun exposed slopes and around cornices.
Confidence
Moderate - Timing or intensity of solar radiation is uncertain
Weather Forecast
A ridge of high pressure keeps the region dry Thursday and Friday before a weak storm system arrives Saturday. Thursday is expected to be mainly sunny with light alpine winds from the southwest to west. Freezing levels are expected to drop below valley bottom overnight and reach 1700-2000m on Thursday afternoon. Friday is expected to be mainly sunny in the morning with increasing cloudiness during the afternoon. Alpine winds are expected to be light from the southwest but may increase during the afternoon and freezing levels are forecast to reach 2000-2500m. There is still a lot of uncertainty as to how warm it will get on Friday. A weak storm front is currently forecast to reach the region Friday overnight bringing 5-10cm of snowfall on Saturday.
Avalanche Summary
On Tuesday, a natural size 2 slab avalanche was reported from a gulley side wall feature on an east aspect at 2000m. This released down 80cm. Two natural size 1.5 storm slab avalanches were reported from northwest through northeast aspects at 2600m and released down 40cm. Numerous solar triggered loose avalanches up to size 2 were reported from steep south-facing slopes in the alpine. A natural size 3 cornice release was also reported from a northwest aspect at 2650m. Ski cutting produced several size 1 soft wind slabs from immediate leeward features. Explosives triggered a large cornice which released a size 2.5 persistent slab on a weak layer down 140cm on a northeast aspect. On Monday, a few size 1 ski cuts were reported from steep convex features. These were on an east aspect at treeline and were 20-40cm thick. Skier triggered sluffing from steep terrain features below treeline was also reported.
Snowpack Summary
A sun crust exists on south facing slopes at all elevations. Thin wind slabs are being reported in leeward features in the alpine and large cornices remain a concern, especially during the heat of the day. The surface hoar and/or crust layer from early February is now down 40-70cm and has been responsible for some large avalanches recently. This layer is expected to become most reactive during the heat of the day, especially on sun exposed slopes. The early January surface hoar/ facet layer is typically down 70-120cm. Triggering an avalanche on this layer has become unlikely but it still has isolated potential to produce very large avalanches with a heavy trigger. In general, the lower snowpack is well settled and strong, apart from some thin snowpack areas where basal facets exist.
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.
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.