The ground cools off at night (by radiating heat to space) and in the morning, moist air will encounter the cool ground and water will condense, because at lower temperatures, the air can hold less moisture.
The air can hold only a specific amount of water at any given temperature. As the temperature increases, the amount of water that it can hold also increases. The relative humidity is the amount of water in the air vs the total amount of water that can be held at current temperatures. At night, the temperature of the air decreases, so the amount of water it can hold also decreases. When the temperature drops, and the water present in the air exceeds the maximum amount of water the air can hold, dew forms and falls to the ground.
There is a certain amount of moisture in the air at any given time. There is also a meteorological figure known as the "dewpoint" - the temperature at which moisture in the air condenses out of the air as dew - the dewpoint is dependent upon the moisture content of the air. If the overnight temperature drops below the dewpoint, dew forms.
Dew forms on grass overnight because of condensation. When there is warm and and a cold ground, the water vapor in the air condenses, which causes the dew on the ground. At night, the air is much cooler, which makes the dew on the ground.
Dew forms on a cool morning because water molecules are always moving through the surrounding air. When the temperature drops, this moisture gathers onto something nearby.
Dew is form in the morning due to deposition.
Actually. dew is a rare event in most deserts as the air is much too dry.
Dew forms on grass overnight because the temperature falls or if the two temperatures are close.
We only see dew in the morning because of the way dew forms. For dew to form, air must be cooled to its condensation point. There must be little movement to the air or it will remain mixed and not form dew, but will form fog instead. (Fog is formed in other ways as well). These conditions usually occur overnight, when the winds die down, and the air becomes still. Radiational cooling from the ground or structures near the surface, such as automobiles, mailboxes, etc. cools the air in contact with the ground or structures. The humidity in the air condenses into droplets of moisture we call dew. After sunrise, the ground begins warm up and usually the wind increases. Both these events warm the air and evaporate the dew.
Dew does not form damp and wet conditions.
Well dew is a form of condensation. That being said a dry climate is less likely to produce dew.
Dew
If the temperature of the ground, grass, and other surfaces is warmer than the dew point of the air that comes in contact with the surfaces, dew will not form. Sometimes this happens when the air is really dry and the dew point is very low.
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Dew
dew point
Water droplets condensed from the air, usually at night, onto cool surfaces
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That depends entirely upon where you are in the world but dew is unconnected to time of year as such. It forms when it cools enough at night for the RH to get to 100%. In some parts of the world that could be every night, in others never or very rarely.
When dew forms in the winter, it forms at night and its colder at night so the dew freezes at that point in freezing.
High air humidity, low temperature and absence of sunshine during night with minimum air velocity are needed to form dew. These things are very common during autumn and spring seasons causing maximum dew formation.
The air near the ground cools to the DEW POINT.