Five distinct and common examples of condensation occurring in nature and everyday life include the following physical phenomena. First, the formation of morning dew on grass and garden vegetation when the ground cools down and causes moisture in the surrounding air to liquefy on cool surfaces. Second, water droplets collecting on the outer surface of a cold beverage glass or soda can during a hot day as warm atmospheric humidity hits the chilled container. Third, bathroom mirrors and tiles steaming up and developing water streaks during a hot shower when humid vapor encounters cooler glass and ceramic surfaces. Fourth, clouds forming high in the Earth atmosphere as warm, moist air rises, expands, and cools adiabatically at higher altitudes, causing water vapor to condense around microscopic particles. Fifth, breath turning into a visible white mist or fog on a freezing winter day when warm, moist exhaled air instantly condenses upon meeting the sub-zero outdoor temperature. These examples demonstrate how temperature differentials reliably trigger the transition of invisible airborne vapor into visible liquid water.
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