Sleet is a form of precipitation that occurs when raindrops freeze into small ice pellets before reaching the ground. It is commonly observed during winter weather conditions, particularly when the air temperature is near freezing. Sleet is different from freezing rain, which falls as liquid rain and freezes upon contact with surfaces, creating a layer of ice.
Sleet forms when a layer of warm air exists between layers of cold air. As snow falls through the cold air layer, it melts into rain. The rain then passes through a shallow layer of cold air near the ground, causing it to refreeze into ice pellets before reaching the surface.