Molecular-Scale Temperature

The molecular-scale temperature is the defining property of the U.S. Standard Atmosphere, 1962. It is defined by the relationship:

[math]\displaystyle{ T_m(z)=\frac{M_0}{M(z)}\cdot{T(z)} }[/math]

T_m(z) is molecular-scale temperature at altitude z;

M₀ is molecular weight of air at sea level;

M(z) is molecular weight of air at altitude z;

T(z) is absolute temperature at altitude z.

This is citation of the Technical Report of United States Air Force from 1967. ^[1]

References

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