The main problem was soft slabs formed within the storm snow, both from high precipitation rates during the early part of the storm and wind drifting. The wind increased through the day and the new snow seemed to be getting more sensitive later in the day. The weather was very warm before the cold front hit last night so the pre-existing snow was fairly damp and the new snow bonded well to it. But there are some weak layers within the new snow, both in the dirt layer at the base of the new snow and a little higher up when the high precipitation intensity was occurring.

The ski areas still open are reporting control results this morning of widespread, sensitive soft slabs that ran fast and far, as if often the case with very low density new snow sliding on an ice crust and density inversions within the new snow. Activity settled out by about mid day but increasing wind later in the day is probably creating more wind slabs in upper elevation, wind exposed terrain. With the very poor visibility due to heavy snow through the day, it was hard to tell what ran and what did not. Hopefully, tomorrow we can see more.

On Thursday, it's supposed to be cloudy in the morning but it looks like the sun will shine through in the afternoon and the temperatures rise. So watch for cold, dry snow turning damp in a hurry, which could initiate rollerballs and damp sluffs.