The magnitude of the decrease of an atmospheric parameter (principally pressure, temperature or moisture). For example, the standard temperature lapse rate in the lower atmosphere is 2.0° C per 1000 ft.
the decrease of temperature with height in the atmosphere. Confusingly, the opposite case, an increase in temperature with height, is known as a negative lapse rate.
Change of an atmospheric variable (temperature unless specified otherwise) with height.
The rate at which temperature decreases with height. The average lapse rate in the troposphere is 3°F per 1,000ft, but the actual rate varies a good deal between the two extreme conditions of dry and saturated air.
The rapidity with which temperature decreases with altitude. The normal lapse rate is defined to be 3.6 degrees F per 1000 feet change in altitude. The dry adiabatic lapse rate is about 5.5 degrees F per 1000 feet, and the wet adiabatic lapse rate varies between 2 and 5 degrees F per 1000 feet.
The rate at which temperature decreases in a rising and expanding air parcel.
The vertical temperature gradient above the earth's surface; that corresponding to adiabatic expansion of rising air is a reduction of 0.6° K per 100 m.
rate at which the air cools with altitude change.
the rate of temperature decrease with increase in altitude
the rate of change of temperature with height
Temperature decreases with altitude. The rate of decrease is the lapse rate. The average rate is 3-1/2 degrees F per 1000 feet of increased height. The rate is different in moist air and dry air.
The decrease of an atmospheric variable with height, the variable being temperature, unless otherwise specified.
The change in temperature associated with a change in elevation. When climbing a mountain, the temperature falls approximately 1°C for every 100m in altitude gained.
The decrease of temperature with height, considered positive when temperature decreases with height.
The change in temperature with altitude in the atmosphere.
(- The change of temperature with a change in height. Also a rate of cooling. A positive lapse rate indicates temperatures cooling as height increases while a negative lapse rate indicates an inversion.
The change in temperature as you increase in altitude. A strong lapse rate means an unstable atmosphere.
The rate at which temperature decreases with increasing height. The standard atmosphere assumes a lapse rate of 6.5°C per km up to the base of the stratosphere. The Dry Adiabatic Lapse Rate is 9.8°C/km.
The change of an atmospheric variable, usually temperature, with height. A steep lapse rate implies a rapid decrease in temperature with height and is a sign of instability.
The rate at which air temperature decreases with existing altitude.
The lapse rate is defined as the negative of the rate of change in temperature with height observed while moving upwards through an atmosphere. While typically applied to Earth's atmosphere, the concept can be extended to any gravitationally supported ball of gas.