Cloud water investigations have been performed at the highest elevation of
Central Germany in 1997. Results of extensive trace element measurements ar
e presented. Besides conductivity, pH, liquid water content and major ions
the data set includes 49 minor and trace elements. Estimation of crustal en
richment factors (EFs) provides an indication of the anthropogenic contribu
tions to the cloud water concentrations. The variation of cloud composition
with time has been illustrated for two selected events with different air
mass origins. The chemical composition of the cloud condensation nuclei on
which the droplets grow mainly determines the cloud water chemistry. For a
cloud event in June 1997 the concentrations of the crustally derived elemen
ts Si, Al, Fe, Ti, Ce, La and Nd follow each other closely. The fact that S
O42-, NO3- and NH4+ are only moderately correlated with the particular poll
utants with high enrichment factors such as Cd, Sb, Pb, Zn, Cu, As, Bi, Sn,
Mo, Ni, Tl and V indicates that their source regions are more widespread.
During an event in October 1997 the time trends for most minor and trace el
ements follow rather closely those for the major ions NH4+, SO42- and NO3.
Back trajectories show that the transport from continental and marine Europ
ean sources was the likely cause of the sample concentrations. EFs of trace
elements in cloud water samples during the June and October event show a s
trong correlation with those obtained for urban particulate matter. Althoug
h both events are influenced by air masses of different origin, there is a
good agreement between the EF signatures. (C) 2000 Elsevier Science Ltd. Al
l rights reserved.