Monday's intense precipitation event rain-soaked the existing snowpack up to about 1800 m and left wet snow in place up to 2000 m. Strong to extreme wind on Monday and Tuesday likely created touchy storm slabs, cornices, and wind damaged snow in high elevation alpine terrain. The deepest snow is found at alpine elevations, with depths of 60 to 140 cm. See
this report from Brew Lake and
this report from Shovelnose Creek for an idea of recent conditions. Approximately 50 cm of new snow now lies above a thin rime ice lens formed last weekend. A thicker melt freeze crust can be found 75 to 90 cm below the surface. This crust may be associated with weak faceted crystals in some places where it lies close to the ground. This is most likely to cause problems in glaciated terrain or on smoother, high elevation slopes where the summer snow did not melt out.