A parcel of unsaturated air is cooled at constant pressure till it reaches the temperature at which water starts to condense out of it. We have reached the air’s Saturation Temperature Adiabatic Temperature Freezing Temperature Dew Point Temperature
Question
A parcel of unsaturated air is cooled at constant pressure till it reaches the temperature at which water starts to condense out of it. We have reached the air’s Saturation Temperature Adiabatic Temperature Freezing Temperature Dew Point Temperature
Solution 1
We have reached the air’s Dew Point Temperature.
The dew point temperature is the temperature at which the air can no longer hold all of its water vapor, and some of the water vapor must condense into liquid water. The dew point is always lower than (or equal to) the air temperature.
Solution 2
We have reached the air’s Dew Point Temperature.
The dew point temperature is the temperature at which the air can no longer hold all of its water vapor, and some of the water vapor must condense into liquid water. The dew point is always lower than (or equal to) the air temperature.
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