the realationship between condensation and dew point is that condensation occurs when it reaches the dew point.
Condensation point
Condensation occurs when air reaches its dew point, which is the temperature at which air becomes saturated with moisture and can no longer hold it in gaseous form. When air cools to its dew point, water vapor in the air condenses into liquid water, forming dew or fog.
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dew point temperature. It is the temperature at which the air reaches its saturation point and condensation begins to form, leading to the formation of dew or fog.
The process of air reaching its dew point is called condensation. As the air pressure reaches the dew point, the humidity increases.
Dew point is the temperature at which air becomes saturated with water vapor, causing condensation to form dew. It is a measure of humidity in the air, with higher dew point values indicating more moisture in the atmosphere. Dew point is often used in weather reports to describe how muggy or dry the air feels.
Condensation occurs at dew point temperature which is "the temp. at which first dew from vapours is formed when we are decreasing the temp. of the vapours".
Dew point.
Dew point
The dew point is the temperature where condensation begins.
Condensation occurs in the atmosphere as part of the phases in rain cycle. During the condensation phase, water vapor transforms into liquid form. When warm air rises into the atmosphere, it cools down and loses its ability to hold water vapor resulting to the condensation of water forming cloud droplets.
Yes, it is possible for the dew point to be below freezing. Dew point is the temperature at which air becomes saturated with moisture and condensation forms. If the air is very dry, the dew point can be below freezing, meaning that the air is not saturated with enough moisture for condensation to occur at temperatures above freezing.