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The atmospheric pressure varies proportionally from sea level to height, and the air temperature drops by 6K for every T km i

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d^ mg Earth on the Sutae essure Psesuse ot a heiaht dy from the earth Susta<, Bs fosce balance.df Pse ue decrease as Uve ao avay -from earth nto atmasphere. Form idcol gas euahm m - number 4 meles olecul nnass m RT RT PMRT 二〇 (Since ontne earm he ic- RT 又 (ok aru heiat im ?a = 1.01325 basb)Assuming tempes ature is vacing neary :. Tempesatue at any height from eh sutfae

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