Deposition monitoring may generally serve at least one of the followin
g purposes: (a) determining ecosystems at risk, (b) evaluating tempora
l and spatial trends. (c) developing numerical models, or (d) estimati
ng deposition effects. In this paper, an overview of available knowled
ge about monitoring methods is given. Furthermore, it is tried to illu
strate the (dis)agreement between results obtained using different met
hods. It might be concluded that throughfall, micro meteorological met
hods (supplemented/supported by inference) and watershed balance metho
ds (S saturated systems) yield similar estimates of the annual mean to
tal deposition of sulphur, within generally acceptable uncertainly lim
its (approximately 30%). A larger uncertainty exists to estimate reduc
ed or oxidised nitrogen and base cation fluxes. It is clear that for i
ndividual ecosystems deposition in general, and dry deposition in part
icular, can still not be quantified with sufficient accuracy. The vari
ous methods have different advantages and drawbacks and the choice of
a certain method for estimation of the flux of a specific pollutant to
a specific ecosystem may in many cases depend on the purpose of the s
tudy and on requirements on accuracy and costs.