The dry adiabatic lapse rate is the rate at which the temperature of an unsaturated air parcel decreases with an increase in altitude, typically at about 9.8°C per kilometer. This concept is crucial for understanding atmospheric stability, buoyancy, and how air parcels behave when they rise or sink in the atmosphere, playing a vital role in processes like convection and adiabatic cooling.
congrats on reading the definition of dry adiabatic lapse rate. now let's actually learn it.