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moist adiabatic lapse rate

Submitted by Anonymous (not verified) on

Rate of decrease of temperature with increasing height of an air parcel lifted at saturation via adiabatic process through an atmosphere in hydrostatic equilibrium. Rate varies according to the amount of water vapor in the parcel and is usually between 2.0 and 5.0 degrees F per 1000 feet (3.6 and 9.2 degrees C per 1000 meters). 

vectors

Submitted by Anonymous (not verified) on

Directions of fire spread as related to rate of spread calculations (in degrees from upslope).

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