Use equations (1.39) and (1.40) on p. 26 in the textbook to derive the following expression for adiabatic expansion of an ideal gas. (Hint: use the relation d(aln x) = a dx/x.)
(dT)/(dP) = (2)/(f+2)(T)/(P)
Combine this relation with the barometric equation to calculate the dry adiabatic lapse rate, d(T)/(d)z, for Earth's troposphere in units of (K)/(km). (Note you are not solving for anything, but just trying to derive the equation)
VTf/2 = constant.
(1.39) VP = constant,
(1.40)