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