Analysis of the chemical composition of rain at high temporal resoluti
on provides additional information on wet deposition processes. High r
esolution data was obtained using a microprocessor-based acid rain mon
itor at two sites in SW Scotland and SE England. Meteorological detail
s of the transport and wet deposition processes during two frontal rai
n events were examined and related to rainfall composition. Rapid depl
etions of ion concentrations during heavy rainfall in the first event
were interpreted using a rainfall scavenging model. The sub-event data
for the second event showed the influence of frontal discontinuities.
Increasing ionic concentrations during this second event were attribu
ted both to the change in air mass, and to diminished upwind precipita
tion scavenging.