The wet adiabatic lapse rate cools faster with rising altitude than the dry adiabatic lapse rate.

Name: The wet adiabatic lapse rate cools faster with rising altitude than the dry adiabatic lapse rate.
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The wet adiabatic lapse rate is slower than the dry adiabatic lapse rate because the process of condensation in a rising parcel of air releases latent heat, which reduces the rate at which the air cools as it ascends.

The Wet Adiabatic Lapse Rate Cools Faster with Rising Altitude