The barometric formula, relating the pressure p(z) of an isothermal, i
deal gas of molecular mass m at some height z to its pressure p(0) at
height z=0, is discussed. After a brief historical review, several der
ivations are given. Generalizations of the barometric formula for a no
nuniform gravitational field and for a vertical temperature gradient a
re also presented. (C) 1997 American Association of Physics Teachers.