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Which profile does pressure follow in an isothermal atmosphere?

  • A.An exponential decrease with height
  • B.A linear decrease with height at a rate determined by the density of the air at the surface beneath it
  • C.A parabolic decrease
  • D.A decrease proportional to the square root of the height above the surface at which the profile begins

Answer: A

Integrating the hydrostatic equation with constant temperature gives pressure proportional to the exponential of minus height over scale height. Real atmospheres are not isothermal but the exponential form is an excellent first approximation over a few kilometres. A linear decrease would be correct only for constant density, which the atmosphere emphatically is not. Most errors here come from carrying a result across from a neighbouring case where it does not hold.

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