A dew drop is a tiny drop of water that appears on objects in the morning or evening due to condensation. As the surface cools, atmospheric moisture condenses at a rate greater than that of which it can evaporate.
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Dew is water droplets that form on surfaces like grass or leaves during the night when the air cools down and reaches its dew point temperature, causing moisture to condense. Dew is typically visible in the morning and can be important for plant survival in dry environments.
Tiny drops of water that form on cool surfaces when atmospheric vapor condenses.
Dew is water and water can freeze. So yes, dew can freeze.
The temperature at which moist air becomes saturated and forms dew is called the dew point temperature.
If there is no dew on the grass in the morning, it means that it did not get cold enough to condense the water vapor in the air. The dew point, the temperature at which dew forms, depends on the humidity: if it is very humid, dew will form at a relatively warm temperature, but if it is very dry, dew will not form until it gets quite chilly.
A dewdrop would drop the amount of dew it carries, which is usually a small amount. The size of the dewdrop and the atmospheric conditions will affect how much dew it can hold before falling.
"Dew" in French is translated as "rosée".