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Whether or not water vapor will condense into droplets depends on the temperature. The temperature at which droplets can form is called the Dew Point. When surface temperature drops, eventually réaching the dew point, atmospheric water vapor condenses to form small droplets on the surface. This process distinguishes dew from those hydrometeors (metéorological occurrences of water) which are formed directly in air cooling to its dew point (typically around condensation nuclei) such as fog or clouds. The thermodynamic principles of formation, however, are virtually the same.

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