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 - Due to the number of field observations
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 5-10cm 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
On Tuesday, several large (size 3) avalanches were reported from south-facing slopes near Golden. The avalanches were thought to be solar-triggered and could have failed on any of the persistent weak layers mentioned in the snowpack discussion section. At the time of publishing no new avalanches were 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. 30-70 cm recent storm snow overlies a prominent weak layer buried on or around Feb-27. The deepest snow amounts appear to be in the west central area near Kootenay Lake. The Feb-27 weak layer comprises surface hoar and a crust. It has been widely reported but recent snowpack test results are mixed, with some tests indicating this layer is gaining strength, while others indicating it can still fail with sudden "pop" results. A deeper weak layer from mid-February is now down 50-80cm. The early January surface hoar/facet layer is typically down 70-120cm. Triggering an avalanche on either of these layers has become unlikely but either still has the isolated potential to produce very large avalanches with a heavy trigger.
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.