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The lapse rate from 126 to 175 km is +10.0Â°C km -1; temperature at 175 km is 539.7Â°C (molecular-scale temperatures). 1  The U.S. Extension to the ICAO Standard Atmosphere is essentially a recomputation of the above data from the surface to 300 km.2  See air.he lapse rate from 126 to 175 km is +10.0Â°C km -1; temperature at 175 km is 539.7Â°C (molecular-scale temperatures). 1  The U.S. Extension to the ICAO Standard Atmosphere is essentially a recomputation of the above data from the surface to 300 km. 2  See air.
This lapse rate varies strongly with temperature. A typical value is around 5 Â°C/km (2.7 Â°F/1,000 ft or 1.51 Â°C/1,000 ft). The reason for the difference between the dry and moist adiabatic lapse rate values is that latent heat is released when water condenses, thus decreasing the rate of temperature drop as altitude increases. This heat release process is an important source of energy in the development of thunderstorms.