Most slopes have entered a
daily melt-freeze cycle, with the exception of north-facing slopes above 2000 m. On these colder slopes, you may find 10-20 cm of dry powder or isolated wind slabs. These same slopes may also have a layer of faceted grains buried 30 to 50 cm below the surface, but this layer that has shown signs of strengthening. Elsewhere, the surface has been melting each day and then freezing into a hard crust overnight. The mid snowpack is generally strong, but the base of the snowpack is composed of faceted snow that is capable of producing very large avalanches during times of intense warming (such as last week).Snow is disappearing rapidly at lower elevations.