The moist adiabatic lapse rate varies strongly with temperature.
2.
Above that altitude, the adiabatic lapse rate decreases to the moist adiabatic lapse rate as the air continues to rise.
3.
The lapse rate, dry adiabatic lapse rate ( DALR ) and moist adiabatic lapse rate ( MALR ), are obtained.
4.
The moist adiabatic lapse rate varies from 1.1 �C to 2.8 �C ( 2 �F to 5 �F ) per 1, 000 vertical feet.
5.
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 ).
6.
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.
7.
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 ).
8.
Although all the datasets show the expected tropospheric amplification at seasonal and annual timescales it is still debated whether or not the long term trends are consistent with the expected moist adiabatic lapse rate amplification due to difficulty of producing homogenized datasets, some satellite temperature reconstruction are consistent with the expected amplification while others are not.
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