Warmer air can hold more water than colder air. The air cools during the night due to lack of sunshine, and when it gets so cool that it can't hold any more water (called the dew point), dew forms (or frost if the temperature is below freezing). After sunrise, the air starts warming up. That makes it able to hold more water, so the dew evaporates.
When the sun rises, its warmth causes the dew on surfaces to evaporate. This process is known as evaporation, where the liquid water from the dew turns into water vapor and is released into the atmosphere.
It evaporates.
when the day gets warmer dew melts
As water vapor cools to the dew point it converts from a gas back to a liquid.
rain comes
when air contains as much water vapor as it can . it said to be structured and condensation can occur. the temperature at wich this takes place is called the dew point.
what forms when air rises cools a dew point and then becomes saturated
Typically on any cooling surface in a humid environment. For example, leaves warmed by the sunlight during the day, will collect condensed moisture (dew) as they cool during the evening. When the sun rises and re-heats the leaves, the dew will eventually evaporate.
Dew-Dew-Dewey Day was created in 1927.
When the temperature comes down to the dew point, the air can support no more water vapour and the dew begins to to form. Air can absorb more water vapour as the temperature rises, so the difference between the dew point and the actual temperature gives a measure of the humidity.
The level of dew point temperature at which the clouds condense rises during the day.Hence the bases of the clouds will be higher at day time.
Because the temperature changes and the dew point is dependent on the temperature.
Dew appears on grass in the early morning hours. It goes away after the sun is up because the heat of the sun causes the water to evaporate.