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The temperature of the troposphere generally decreases as altitude increases. The rate at which the temperature decreases, â d T / d z {\displaystyle -dT/dz} , is called the environmental lapse rate (ELR).
Thus vertical air motions act to heat the lower atmosphere and cool the higher. The combined effect of those, as a few people mentioned, is that temperature on the average decreases with altitude in the troposphere-at a rate of 6.5 Â°C per km (3.6 Â°F per 1000 ft.). Yet the lapse rate varies depending on conditions.