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{{Orphan|date=October 2012}}
 
The '''molecular-scale temperature''' is the defining property of the [[U.S. Standard Atmosphere#1962 version|U.S. Standard Atmosphere, 1962]]. It is  defined by the relationship:
 
: <math>T_m(z)=\frac{M_0}{M(z)}\cdot{T(z)}</math>
 
: ''T<sub>m</sub>(z)'' is molecular-scale temperature at [[altitude]] ''z'';
: ''M<sub>0</sub>'' is [[molecular mass|molecular weight]] of air at [[sea level]];
: ''M(z)'' is molecular weight of air at altitude ''z'';
: ''T(z)'' is [[Thermodynamic temperature|absolute temperature]] at altitude ''z''.
 
This is citation of the Technical Report of [[United States Air Force|USAF]] from 1967.
<ref>{{cite book
| last          = Brackbill
| first        = Jeremiah U.
| first2        = Edmund A.
| last2        = Nawrocki
| first3        = William A.
| last3        = Whitaker
| title        = Atmospheric models for use in hydrodynamic computer codes
| url          = http://www.dtic.mil/cgi-bin/GetTRDoc?AD=AD0818407
| format        = pdf
| accessdate    = 2012-05-30
| series        = AFWL-TR-67-75
|date=August 1967
| publisher    = Air Force Weapons Laboratory. Research And Technology Division. Air Force Systems Command
| location      = [[Kirtland Air Force Base]], [[New Mexico]] (USA)
}}</ref>
 
==References==
{{reflist}}
 
[[Category:Atmosphere| ]]
[[Category:Temperature]]
 
{{climate-stub}}

Revision as of 04:49, 26 May 2013

Template:Orphan

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

Tm(z)=M0M(z)T(z)
Tm(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. [1]

References

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