During cold weather, not only does the temperature near the ground play a role in what type of precipitation falls, but the temperature above the surface can be critical to our precipitation type.
When temperatures are below freezing from the surface upward into the atmosphere, precipitation falls as snow.
Sometimes the section of the atmosphere above the surface and below the clouds may warm above freezing. As snow falls, it enters an area of temperatures above freezing and melts the snow. This layer of cold air near the ground refreezes the rain and forms sleet.