The distribution of precipitation and wet deposition of pollutants by rain
and snow in the western Sudete mountains in Poland has been investigated bo
th for selected event case studies and for a longer term period of monitori
ng. The results were compared with a numerical model of two-dimensional air
flow and scavenging of cap cloud by precipitation. The results of both mode
lling and analysis of case studies during north-westerly flow indicate that
the first orographic barrier (Stog Izerski) receives the highest depositio
n and acts to "shield" downstream hills (Szrenica). The "seeder-feeder effe
ct" typically caused an increase in precipitation at Stog Izerski of about
50% relative to the upstream lowlands. Ion concentrations in cloud and rime
water were consistently higher than those in rain and snow water. Spatial
variations in deposition by snow were found by the model not to be as signi
ficant as those for rain due to the slow fall speeds of snow crystals and t
heir greater horizontal transport. The monitoring studies showed a maximum
in sulphate and nitrate deposition at Stog Izerski. (C) 1999 Elsevier Scien
ce Ltd. All rights reserved.