D. Fowler et al., QUANTIFYING THE FINE-SCALE (1KMX1KM) EXPOSURE AND EFFECTS OF OZONE .1. METHODOLOGY AND APPLICATION FOR EFFECTS ON FORESTS, Water, air and soil pollution, 85(3), 1995, pp. 1479-1484
Surface ozone concentrations show very large local variability. This,
in rural areas, is largely a consequence of the degree to which the su
rface air is decoupled from the bulk of the atmosphere by nocturnal an
d winter stability effects and of the aerodynamic roughness and topogr
aphy of the countryside. Procedures have been developed to simulate th
ese effects and have been used with O-3 data from a regional monitorin
g network to quantify exposure of vegetation to mean and peak O-3 conc
entrations. The index of exposure to potentially phytotoxic O-3 concen
trations is the AOT40 (accumulated exposure over a threshold of 40 ppb
) expressed in ppb.h. The accumulated exposure of crop and forest surf
aces to ozone is shown to increase approximately linearly with altitud
e and along a gradient: from 3000 ppb.h in north west Scotland to 7000
ppb.h in the south of England. The area of UK forest which exceeds th
e critical level for ozone effects (10(4) ppb.h above 40 ppb) totals 2
.0 x 10(4) km(2) and represents 47% of afforested land. The areas affe
cted include most of southern and central England and Wales and large
plantation forests of Northumberland and the Scottish borders.