DALR
The Dry Adiabatic Lapse Rate (DALR) is the rate at which the temperature of unsaturated air changes as a parcel ascends or decends through the atmosphere.
The DALR is approximately 9.8 degree Celsius per 1 km.
Deep-layer mean wind ...
DALR
Dry Adiabatic Lapse Rate. The rate at which the temperature of dry (unsaturated) air changes as it is raised or lowered adiabatically through the atmosphere. The DALR is approximately -9.
DALR - permalink - collapse
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Dry Adiabatic Lapse Rate
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DALRDry Adiabatic Lapse RateDamIn hydrologic terms, any artificial barrier which impounds or diverts water. The dam is generally hydrologically significant if it is:
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The dry adiabatic lapse rate (DALR) is the rate at which a rising parcel of unsaturated air, such as a thermal, will lose temperature. Unsaturated air has less than 100% relative humidity, ie it is below its dew point.
The rate at which the temperature of a parcel of dry air decreases as the parcel is lifted in the atmosphere. The dry adiabatic lapse rate (abbreviated DALR) is 5.5?Ǭ?F per 1000 ft or 9.8?Ǭ?C per km.
Dry Crack ...
Dry adiabatic lapse rate: the rate at which the temperature of a parcel of dry air decreases as the parcel is lifted in the atmosphere. The dry adiabatic lapse rate (abbreviated DALR) is 5.5°F per 1000 ft or 9.8°C per km.
E ...
if the air is unsaturated (air temperature > dew point temperature), the cooling/warming will be at a rate of 3 degC per 1000 ft (or 10 degC per 1 km): This is known as the Dry Adiabatic Lapse Rate/DALR; ...
Dynamic lifting causes the mid-levels to cool at a greater rate than the lower troposphere since air in the lower troposphere cools at the WALR and air in the middle troposphere cools at the DALR.
 See also: Meteor, Earth, Humidity, Surface, Lapse Rate
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