A poor overnight refreeze should lead to wet avalanche activity on all but upper elevation northerly aspects. Increased cloud cover may limit activity, but filtered sunshine may quickly warm the snowpack, with human-triggered and isolated natural wet snow avalanches possible. If clouds build up earlier than forecasted, these solar aspects may not soften that much. Additionally, greenhousing and possible rain may induce wet avalanche activity on low elevation northerly aspects.

Fortunately, managing the wet snow avalanche problem is pretty simple - if the snow starts becoming damp, move to a cooler aspect or lower-angled terrain.

This section includes isolated areas of lingering soft slab instabilities, fresh wind drifts up high, and cornice falls. These all warrant some mention for extra caution in the higher elevations, particularly in steep, unforgiving terrain. As Derek mentioned in his report from Friday, cornices still need to be given the proper respect and margin/distance near the ridgelines. Warming temperatures may make these large cornices even more sensitive.