He. Scheel et al., ON THE SPATIAL-DISTRIBUTION AND SEASONAL-VARIATION OF LOWER-TROPOSPHERE OZONE OVER EUROPE, Journal of atmospheric chemistry, 28(1-3), 1997, pp. 11-28
Surface ozone data from 25 European low-altitude sites and mountain si
tes located between 79 degrees N and 28 degrees N were studied. The an
alysis covered the time period March 1989-February 1993. Average summe
r and winter O-3 concentrations in the boundary layer over the contine
nt gave rise to gradients that were strongest in the north-west to sou
th-east direction and west-east direction, respectively. Wintertime O-
3 ranged from 19 to 27 ppb over the continent, compared to about 32 pp
b at the western border, while for summer the continental O-3 values r
anged between 39 and 56 ppb and the oceanic mixing ratios were around
37 ppb. In the lower free troposphere average wintertime O-3 mixing ra
tios were around 38 ppb, with only an 8 ppb difference between 28 degr
ees N and 79 degrees N. For summer the average O-3 levels decreased fr
om about 55 ppb over Central Europe to 32 ppb at 79 degrees N. In addi
tion, O-3 and O-x (= O-3 + NO2) in polluted and clean air were compare
d. The amplitudes of the seasonal ozone variations increased in the no
rth-west to southeast direction, while the time of the annual maximum
was shifted from spring (at the northerly sites) to late summer (at si
tes in Austria and Hungary), which reflected the contribution of photo
chemical ozone production in the lower parts of the troposphere.