In this study CO2 and H2O flux measurements made above a spruce forest
was compared with the ozone flux to the canopy during growing season
1995. The fluxes were determined by micro meteorological gradient meth
ods using a 36-m tall meteorological mast. The trees were about 12 m h
igh and air sampling was done from 36 and 18 m. The preliminary result
s suggest that there is only little correlation between ozone concentr
ation in 36 m and the ozone flux to the forest, but the diurnal patter
n of ozone uptake seems to be significantly influenced by stomatal con
ductance. The cumulative total ozone uptake seems to follow very well
the evapotranspiration. (C) 1998 Elsevier Science Ltd.