Calculating temperature given altitude

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To calculate temperature at various altitudes in the troposphere, the ideal gas law (PV=nRT) is applied, simplifying to P1/P2 = V1/V2 * T1/T2 by canceling out n and R. The volume of air above a given altitude is calculated using the formula for the volume of a sphere, but the main challenge lies in the pressure drop, which follows the barometric equation rather than volume changes. Meteorologists typically use the ICAO Standard atmosphere, which states that temperature decreases at a rate of 0.0065 °C per meter up to 11 km in the temperate zone. This standard provides a baseline but does not account for local atmospheric variations. Understanding these principles is essential for accurate temperature calculations at altitude.
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Homework Statement


I am trying to figure out how to calculate the temperature at any given altitude in the troposphere.

Homework Equations


Let P=air pressure, V=volume of air above a given altitude, n=number of moles of gas, R=the ideal gas constant, T=temperature, and h=height above sea levelX1 and X2 = the value of X at geographic point 1 and point 2.

PV=nRT (the ideal gas law)
Volume of a sphere = 4/3*pi*radius3
Surface area of a sphere = 4*pi*radius2

The Attempt at a Solution


P1/ P2 = V1nRT1 / V2nRT2.

Now, we don't need to know what n and R are, because they are canceled out of the equation. So ignore them. We are now left with P1/P2 = V1/V2 * T1/T2.

V = 4/3*pi*radius of troposphere - (4/3 * pi * (6371.5+h))
V1 / V2 is pretty obvious and can't be simplified.
 
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The main problem that I see with this is that fall off in pressure is governed more by the barometric equation p= p0 exp (–h/A) where A is roughly 7 km, than by an increase in available volume at greater height.

I do not know how meteorologists do this calculation, but the recommendation of the ICAO Standard atmosphere is that the temperature will fall at a constant rate of 0.0065 °C/m up to 11 km altitude in the temperate zone. Obviously that is an "other things being equal" calculation that cannot take account of local atmospheric conditions.
 

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