Persistent weak layer problems remain on northerly aspects above treeline where old hard slabs of wind drifted snow sit on top of underlying weak facets. The primary layer of concern is a layer of facets that formed near the surface before the storm on January 23. Several windy periods since have built stiff hard wind slabs over top of this faceted layer and human triggered avalanches 1-2 feet deep are possible. A less likely, but not impossible scenario would be for an avalanche failing on this weak layer to step down deeper into the snowpack. For these reasons, I'm still leery of upper elevation, wind loaded terrain. Avoid steep slopes just below ridge lines that have smooth, hard slabs of wind drifted snow or that sound or feel hollow underneath.

Looking ahead, any significant snow load, especially if combined with wind, will have the potential to produce large avalanches breaking below the Christmas rain crust and taking out the entire season's snowpack.

Although most other terrain has generally low danger, small, dry loose avalanches are possible if not likely on steep, shady slopes near treeline and below. The size of the slope dictates how much snow will become entrained and if enough is accumulated, these slides can pack a punch. They won't be enough to bury you but they could take you for a ride and carry you into trees or over a cliff. Manage terrain carefully and be aware of where you might end up. Stop at likely trigger points such as convexities or where the slope suddenly get steeper. Stop or get off to the side if the snow starts moving. The main thing is to catch it early and let it slide without you in it.