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Get the Boydton, VA local weather forecast by the hour and the next 10 days.
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This process distinguishes dew from those hydrometeors (meteorological occurrences of water), which form directly in air that has cooled to its dew point (typically around condensation nuclei), such as fog or clouds. The thermodynamic principles of formation, however, are the same. Dew is commonly formed during select times of the day.
The dew point of a given body of air is the temperature to which it must be cooled to become saturated with water vapor. This temperature depends on the pressure and water content of the air. When the air is cooled below the dew point, its moisture capacity is reduced and airborne water vapor will condense to form liquid water known as dew. [1]
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Dew forms outdoors in the early morning after a clear night, when the surface temperature drops below the dew point. It forms most easily on surfaces that are isolated from conducted heat from deep ground, such as grass, leaves, and spider webs. Dew bows will be clearest on fields littered with cobwebs, as may occur in autumn. [3]
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