The difference between the dry adiabatic lapse rate and the rate at which the dew point drops is around per 1, 000 m.
12.
The dry adiabatic lapse rate ( for unsaturated air ) is 3 �C ( 5.4 �F ) per 1, 000 vertical feet.
13.
Meteorologists use radiosondes to measure the environmental lapse rate and compare it to the predicted adiabatic lapse rate to forecast the likelihood that air will rise.
14.
The temperature decreases with the dry adiabatic lapse rate, until it hits the dew point, where water vapor in the air begins to condense.
15.
As a result of the latent heat that is released during water vapor condensation, moist air has a relatively lower adiabatic lapse rate than dry air.
16.
The moist adiabatic lapse rate varies from 1.1 �C to 2.8 �C ( 2 �F to 5 �F ) per 1, 000 vertical feet.
17.
From there on, follow the moist adiabatic lapse rate until the temperature of the parcel reaches the air mass temperature, at the equilibrium level ( EL ).
18.
This decrease is constant for Earth's atmosphere, and is approximately per kilometer ( 0.62 miles ); this is known as the dry adiabatic lapse rate.
19.
If the environmental lapse rate is less than the moist adiabatic lapse rate, the air is absolutely stable rising air will cool faster than the surrounding air and lose buoyancy.
20.
The difference in moist adiabatic lapse rate and the dry rate is the cause of foehn wind phenomenon ( also known as " Chinook winds " in parts of North America ).
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