Molecular-scale temperature

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

${\displaystyle T_{m}(z)={\frac {M_{0}}{M(z)}}\cdot {T(z)}}$

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 USAF from 1967.

References

1. Temperature
2. Thermodynamic temperature
3. Inversion temperature
4. Molecular scale electronics
5. Curie temperature
6. Negative temperature
7. Absolute scale
8. Absolute zero
9. Molecular dynamics
10. Nanotechnology
11. Molecular diffusion
12. Molecular sieve
13. Thermometer
14. Molecular gastronomy
15. Berendsen thermostat
16. Molecule
17. Temperature dependence of viscosity
18. Index of meteorology articles
19. Index of climate change articles
20. Scale height