H. Pleijel et al., GRADIENTS OF OZONE AT A FOREST SITE AND OVER A FIELD CROP - CONSEQUENCES FOR THE AOT40 CONCEPT OF CRITICAL-LEVEL, Water, air and soil pollution, 85(4), 1995, pp. 2033-2038
Ozone concentrations were measured at a wind-exposed edge of a 60 year
-old 15-20 m tall Norway spruce forest in south-west Sweden and simult
aneously over a barley field 5 ion away for 27 days. At the forest sit
e, measurements were performed at 3 and 13 m height 15 m in front of t
he forest edge, at 3 m height 15 m into the forest, and at 3 and 13 m
height 45 m into the forest. Measurements at 3 m were made with three
replicate tubes separated by 10 m. Differences between replicates were
small. At 13 m height, the concentration (24-hr-average) 45 m into th
e forest was 95% of that in front of the forest edge. The average conc
entration at 3 m height did not vary strongly with the distance into t
he forest, but was 86% of that at 13 m in front of the forest edge. Fo
r AOT40 (Accumulated Exposure Over Threshold 40 ppb ozone), the differ
ences between different positions were larger. At the 13 m level the A
OT40 (day and night) was 88% of that in front of the forest 45 m into
the forest. The AOT40 at 3 m was 71% of that at 13 m outside the fores
t. At the crop site, the ozone concentration at 1.1 m (0.1 m above the
canopy), was 78% of that at 9 m (06.00-22.00). The AOT40 at 1.1 m abo
ve the ground, however, was only 50% of that at 9 m, indicating that s
erious errors can arise if ozone monitoring data are used uncorrected
in dose-response relationships based on measurements performed at plan
t height. The ozone concentration for the whole period differed very l
ittle between 9 m height at the crop site and 13 m height at the fores
t site outside the forest during daytime conditions (06.00-22.00). Nig
ht-time (22.00-06.00) values were only 21% at the crop site of those a
t the forest site due to the stronger night inversion development in t
he agricultural environment compared to the wind exposed forest edge.
The results suggest that variations in topography and vegetation are i
mportant to consider when combining ozone monitoring data with dose-re
sponse functions.