A mesoscale meteorological model with passive tracers is applied in order t
o analyze transport from the atmospheric boundary layer to the free troposp
here. The validation of the model against aircraft measurements indicates t
hat the model adequately simulates the tracer distributions in the free tro
posphere as well as in the boundary layer. Budget calculations of passive t
racers are performed in order to estimate the amount of transport in the ar
ea of a frontal system. The results show a very effective uplift associated
in particular with a WCB transporting up to similar to 70% of a passive tr
acer initialized in the boundary layer to the free troposphere within 3 day
s.