No. Dew is water vapor (humidity) coalescing after the ambient temperature drops below the dew point. In psychrometrics, given the temperature and relative humidity (read as a percentage) one can then determine the specific humidity (read as "grains per pound" or GPP (how many grains of water in a pound of air)) as well as the dew point. The dew you see in the morning on the grass and plants in your yard, or on the windshield, etc... is the same scientific principle as the water droplets that form on a glass of ice water. The short version: Air can only hold so much moisture at a given temperature, and if that air is cooled without removing the water, the air will become saturated and dew will form. EG: @ 85° and 60% relative humidity the specific humidity is 108 GPP and the dew point is 69°
Dew is not water vapor dropping from thunderstorms. Dew forms when the air near the ground cools and cannot hold all of its moisture, causing the excess water vapor to condense into liquid water droplets on surfaces like grass or leaves. Thunderstorms involve the condensation of water vapor in the atmosphere to form clouds and precipitation like rain, rather than dew.
Water vapor that has condensed is called dew. Dew forms when the air cools down and reaches its dew point, causing the water vapor to condense into liquid water droplets on surfaces like grass or leaves.
As the air temperature increases with no addition of water vapor, the dew point will stay the same or decrease. The dew point represents the temperature at which air becomes saturated with water vapor, so if there is no additional water vapor added, the dew point will remain constant or decrease as the air temperature increases.
Condensation
When the dew point decreases while the amount of water vapor remains constant, the air temperature is also decreasing. This means the air is cooling down without any change in water vapor content. Eventually, the air temperature will reach the new, lower dew point, and condensation will begin.
When atmospheric temperature drops, water vapor in the air begins to condense into liquid water droplets. These droplets stick to surfaces such as leaves or grass, forming dew. Dew forms as a result of cooling air reaching its dew point temperature, causing water vapor to condense into liquid water.
Water vapor that has condensed is called dew. Dew forms when the air cools down and reaches its dew point, causing the water vapor to condense into liquid water droplets on surfaces like grass or leaves.
As the air temperature increases with no addition of water vapor, the dew point will stay the same or decrease. The dew point represents the temperature at which air becomes saturated with water vapor, so if there is no additional water vapor added, the dew point will remain constant or decrease as the air temperature increases.
dew
dew
As water vapor cools to the dew point it converts from a gas back to a liquid.
Condensation
When the dew point decreases while the amount of water vapor remains constant, the air temperature is also decreasing. This means the air is cooling down without any change in water vapor content. Eventually, the air temperature will reach the new, lower dew point, and condensation will begin.
The Dew Point is a measurement of the water vapor in the air … the Humidity.
water vapor forms a musk,dew,or left over water droplets
Evaporation.
Condensation
Clouds Dew