### abstract

- We suggest a one-dimensional model of pre-cipitation scavenging of soluble gaseous pollutants by non-evaporating and evaporating droplets that is valid for arbitrary initial vertical distribution of soluble trace gases in the atmosphere. It is shown that for low gradients of soluble trace gases in the atmosphere, scavenging of gas-eous pollutants is governed by a linear wave equation that describes propagation of a wave in one direction. The derived equation is solved by the method of characteristics. Scavenging coefficient and the rates of precipitation scav-enging are calculated for wet removal of sulfur dioxide (SO 2) and ammonia (NH 3) using measured initial distri-butions of trace gases. It is shown that scavenging coeffi-cient for arbitrary initial vertical distribution of soluble trace gases in the atmosphere is non-stationary and height-dependent. In case of exponential initial distribution of soluble trace gases in the atmosphere, scavenging coeffi-cient for non-evaporating droplets in the region between the ground and the position of a scavenging front is a product of rainfall rate, solubility parameter, and the growth constant in the formula for the initial profile of a soluble trace gas in the atmosphere. This expression yields the same estimate of scavenging coefficient for sulfur dioxide scavenging by rain as field estimates presented in McMahon and Denison (1979). It is demonstrated that the smaller the slope of the concentration profile the higher the value of a scavenging coefficient. u Terminal velocity of droplet, cm s -1 U ''wash-down'' front velocity, cm s -1 U 0 ''wash-down'' front velocity for non-evaporating droplets, cm s -1 x (G) Mole fraction of a soluble trace gas in gaseous phase z Vertical coordinate, cm Greek symbols b Coefficient of mass transfer, cm s -1 / L Volume fraction of droplets in air s ch Characteristic time of concentration change in gaseous phase, s s D Characteristic time of diffusion, s K Scavenging coefficient, s -1