Meteorology

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Dry Adiabatic Lapse Rate

Also from: DALR

The dry adiabatic lapse rate refers to the temperature change in a parcel of unsaturated air as it rises (or the pressure is reduced). The reduction in pressure allows the air to expand, and therefore cool.

DALR ≈ 3° / 1,000'

See also

Saturated Adiabatic Lapse Rate

Categories: Meteorology

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