Snow surfaces are highly variable. On higher North aspects (above 1700 m) you may find some dry, faceted snow. Some of this has been redistributed by southwesterly and northerly winds, potentially creating some unusual wind slabs. On solar aspects (East, South, West) the upper 10-30 cm is moist but re-freezes overnight into a solid crust. Most solar slopes at lower elevations are becoming
isothermal. The snowpack has gone through a lot of change with the hot and sunny weather. With forecast freezing levels and air temperatures dropping, the mushy snowpack will start to solidify and lock-up allowing for hard conditions and less avalanche activity, especially on the solar slopes.