The solid form of precipitation produced by the sublimation of water vapour is called "snow."
Snow forms when water vapour in the atmosphere undergoes sublimation directly from a gaseous state to a solid state without passing through the liquid phase. This occurs when the temperature is below freezing (0 degrees Celsius or 32 degrees Fahrenheit) and the relative humidity is high enough for water vapor to condense into ice crystals.
During sublimation, water molecules transform directly from a gas to a solid without becoming liquid. The resulting ice crystals in the form of snowflakes are intricate and unique in shape, reflecting the conditions present during their formation. These delicate ice crystals can join together in the atmosphere and fall to the ground as snow, creating the characteristic white blanket of frozen precipitation we often associate with winter weather.
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