The timing and intensity of solar radiation on Friday is uncertain. If the sun makes an appearance, the snowpack could destabilize quickly and the Avalanche Danger may be HIGH.
Confidence
Moderate - Timing or intensity of solar radiation is uncertain on Friday
Weather Forecast
A ridge of high pressure will keep the region mainly dry and sunny for the early part of Friday. Over the weekend a series of frontal systems will make their way across the region bringing 5-15cm of new snow each day. Ridgetop winds will be light on Friday, increasing to moderate and southwesterly for the weekend. Freezing levels will hover around 1500m on Friday, climb to about 1800m on Saturday, and then drop to about 1500m by Sunday.
Avalanche Summary
No new avalanches have been reported, but I'm sure that speaks more to the lack of observations rather than actual conditions. I expect a good round of wind/storm slab activity took place in response to new snow and strong winds on Thursday. I also expect ongoing potential for human triggering on Friday. Sun may also be the driver for avalanche activity on Friday. With that, you can add cornices and loose wet avalanches to the mix. Solar warming will also increase the likelihood of avalanches failing on deeper persistent layers.
Snowpack Summary
Snowfall accumulations on Thursday were in the 10-20cm range. Strong southerly winds redistributed these accumulations into touchy wind slabs at treeline and in the alpine. At elevations above around 1600 m, approximately 50-80 cm snow rests above a prominent weak layer buried on or around February 27. This weak layer comprises surface hoar sitting on a crust and is reported to be most prominent at sheltered treeline elevations. A couple of sun crusts might exist in the upper 50-70cm on southerly aspects.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.
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.
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.