“…The present version uses Pasquill-Gifford dispersion coefficients, sigma y and sigma z, calculated using McMullen•s [28] method. The atmospheric stability used in the calculations is adjusted to account for enhanced dispersion observed in complex terrain situations by a number of other investigators[20,[29][30][31]. The resulting concentration calculations are adjusted for standard pressure and temperature.InputsThe subroutine requires information on the coordinates of the receptor and source, the plume centerline height, source strength, wind velocity, dispersion coefficients, atmospheric temperature, and atmospheric pressure.…”