The Acid Deposition and Oxidant Model (ADOM) is an Eulerian long-range
transport and deposition model. One of the most highly parameterized
and least well established parts of the model is the scavenging module
that describes cloud formation, pollutant scavenging, aqueous-phase c
hemistry and wet deposition. As a means of gaining insight into the sc
avenging module, results from simulations with the module are compared
with the results from simulations for equivalent conditions with a th
ree-dimensional dynamic cloud chemistry model. Comparisons of results
for a variety of initial conditions show that wet deposition of sulpha
te, nitrate and ammonium ions tend to be underpredicted by the scaveng
ing module and that the pH of the rain is overpredicted. Although the
differences are for the most part not large, they are sensitive to clo
ud top height. The amount of hydrogen peroxide deposited at the surfac
e is significantly smaller in the ADOM module than in the cloud chemis
try model. For the particular conditions that are considered, oxidatio
n is limited by the hydrogen peroxide concentration for the cloud chem
istry model, but by the sulphur dioxide concentration for the ADOM mod
ule.