The difference between the dry adiabatic rate and the moist adiabatic rate is on account of

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The dry adiabatic rate is the rate at which dry air cools or warms as it rises or descends in the atmosphere without any water vapor condensing or evaporating. The moist adiabatic rate is the rate at which moist air cools or warms as it rises or descends in the atmosphere with water vapor condensing or evaporating. The difference between the two is on account of the latent heat of condensation, which is released or absorbed when water vapor condenses or evaporates, respectively. This latent heat affects the rate at which moist air cools or warms, making it slower than the dry adiabatic rate.

The Difference Between the Dry Adiabatic Rate and the Moist