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