A model has been developed to estimate stomatal ozone flux across Europe Fo
r a number of important species. An initial application of this model is il
lustrated for two species, wheat and beech, The model calculates ozone flux
using European Monitoring and Evaluation Programme (EMEP) model ozone conc
entrations in combination with estimates of the atmospheric, boundary layer
and stomatal resistances to ozone transfer. The model simulates the effect
of phenology, irradiance, temperature, vapour pressure deficit and soil mo
isture deficit on stomatal conductance. These species-specific microclimati
c parameters are derived from meteorological data provided by the Norwegian
Meteorological Institute (DNMI), together with detailed land-use and soil
type maps assembled at the Stockholm Environment Institute (SEI). Modelled
fluxes are presented as mean monthly flux maps and compared with maps descr
ibing equivalent values of AOT40 (accumulated exposure over threshold of 40
ppb or nl l(-1)), highlighting the spatial differences between these two i
ndices. In many cases high ozone fluxes were modelled in association with o
nly moderate AOT40 values. The factors most important in limiting ozone upt
ake under the model assumptions were vapour pressure deficit (VPD), soil mo
isture deficit (for Mediterranean regions in particular) and phenology. The
limiting effect of VPD on ozone uptake was especially apparent, since high
VPDs resulting in stomatal closure tended to co-occur with high ozone conc
entrations. Although further work is needed to link the ozone uptake and de
position model components, and to validate the model with field measurement
s, the present results give a clear indication of the possible implications
of adopting a flux-based approach for future policy evaluation. (C) 2000 E
lsevier Science Ltd. All rights reserved.