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From the Rolls-Royce experimental archive: a quarter of a million communications from Rolls-Royce, 1906 to 1960's. Documents from the Sir Henry Royce Memorial Foundation (SHRMF).
Mathematical formulas for calculating temperature and density ratios at altitude.

Identifier  ExFiles\Box 149a\2\  scan0330
Date  13th January 1936
  
-3-
Hs{Lord Ernest Hives - Chair}/Std.1/JH.13.1.36.

Let B = temp. for boiling to take place at altitude.
" r = ratio of density at altitude / density at ground level.

Assuming that system is vented to atmosphere without any pressure valve.

∴ TG = 100 - ΔG (sea level, H being dissipation)
and TA = B - ΔA
at altitude, heat to be dissapted = H(.167 + .834k)
from a

∴ ΔA = ΔG (.167 + .834k) / r .83

= (100 - TG) (.167 + .834k) / r .83

∴ TA = B - (100-TG) (.167 + .834k) / r .83 -----(b)

Let TC = altitude corrected critical AIR temp. :- °C
tA = air temp. at altitude. :- °C
tG = " " " sea level. :- °C

From curves on sheet(1)
We have the following relationships:-
(1) tA = tG - h/500 = tG - .002h.
(2) B = 100 - .001h.
(3) k = 1 - .00003h.
(4) r = 1 - .000025h. } h = altitude in ft

TC = TA + tG
= TA + .002h (from(1))
  
  


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