Snow level and freezing level are not identical
The freezing level marks where air temperature is around 0 °C. Snow can reach lower elevations during intense precipitation, in dry air or where cold air is trapped near the ground.
Why valleys differ
Exposure, ventilation, precipitation intensity and pools of cold air can create substantial local differences.
From lake to mountain
Rain on the shore can coexist with winter conditions on nearby roads and hiking routes at higher elevations. Always check the elevation of your destination.
Safety note
Como Lake Weather is an information service. For warnings, emergencies and safety decisions always consult Civil Protection, Regione Lombardia and the competent authorities.