1. The moist adiabatic lapse rate varies strongly with temperature. 2. Note that adiabatic lapse rate redirects to the lapse rate article you linked. 3. Above that altitude, the adiabatic lapse rate decreases to the moist adiabatic lapse rate as the air continues to rise. 4. Above that altitude, the adiabatic lapse rate decreases to the moist adiabatic lapse rate as the air continues to rise. 5. As the air descends on the leeward side, it is warmed by adiabatic compression at the dry adiabatic lapse rate . 6. Instability results from difference between the adiabatic lapse rate of an air mass and the ambient lapse rate in the atmosphere. 7. The lapse rate, dry adiabatic lapse rate ( DALR ) and moist adiabatic lapse rate ( MALR ), are obtained. 8. The lapse rate, dry adiabatic lapse rate ( DALR ) and moist adiabatic lapse rate ( MALR ), are obtained. 9. A rise from sea level into the upper regions of the atmosphere causes the temperature to decrease ( see adiabatic lapse rate ). 10. The adiabatic lapse rate is the rate at which a rising or falling air mass lowers or increases per distance of vertical displacement.
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