Water In The Atmosphere
Dew point is that state of temperature at which the moist air begins to condense.
It is closely related to the amount of moisture because, the rate of condensation depends upon the amount of relative humidity. If the relative humidity is higher, the condensation needs a slight amount of cooling. On the other hand, when the relative humidity is low, condensation needs a greater amount of cooling.
Sponsor Area
Sponsor Area
Sponsor Area