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Some sort of precipitation occurs when air reaches the dew point. You might get dew, frost, rain or snow.
The process of air reaching its dew point is called condensation. As the air pressure reaches the dew point, the humidity increases.
When the air temperature reaches the dew point, water droplets that are in the air become visible. This is how you would get fog. Relative Humidity goes soaring to near 100%.
saturated
When air evaporates it absorbs the heat of evaporation of water from the air, thus cooling it. When the air is at or below the dew point temperature, water no longer freely evaporates from it; thus this heat is no longer being absorbed from the air.
Some sort of precipitation occurs when air reaches the dew point. You might get dew, frost, rain or snow.
Condensation begins
The process of air reaching its dew point is called condensation. As the air pressure reaches the dew point, the humidity increases.
Saturation
when the temperature reaches the dew point.
the parcel of the air rises high emough , it will eventually cool to its dew point . the process of condensation begins . from this point on as the air rises , laten heat of condensat5ion stored in the water vapor will be released :)
When a paracel of air is cooled to the temperature at which it is saturated, it has reached its dew point.
An air parcel is an imaginary body of air with the basic properties of atmospheric air.
An air parcel is an imaginary body of air with the basic properties of atmospheric air.
dew point
dew point
when the temperature reaches the dew point.