Smog may be contributing to the decline of sugar maples, one of Northeast Ohio's iconic trees — and our high-mileage lifestyle is a big cause
By Mary Topa, PhD
Director of Research, The Holden Arboretum
Tropospheric or ground-level ozone is the primary constituent of smog, and it is the most widespread phytotoxic air pollutant in the United States. Unlike ozone in the upper atmosphere (stratosphere), which has a beneficial effect of it shielding us from the harmful effects of UV radiation, tropospheric ozone probably has the most negative impact of all air pollutants on tree health and growth.
On average, tropospheric ozone is increasing at 0.5–1 percent per year. However, tropospheric ozone is considered a regional pollutant, and urban areas are major sources of ozone precursors that can travel hundreds or thousands of kilometers.
Trees in the urban landscape and in rural communities or in forests downwind of major metropolitan areas are often subjected to some of the highest levels of smog during peak season. Known as a summertime pollutant, tropospheric ozone is a gas composed of three oxygen atoms (O3), and is a product of a photochemical reaction between oxides of nitrogen and volatile organic compounds (VOCs) in the presence of sunlight. Consequently, tropospheric ozone levels are highest on hot sunny days, peaking generally between noon and 7 p.m. Since vehicles can account for as much as half of the VOCs and oxides of nitrogen, areas in moderate non-attainment or worse status, such as the Cleveland/Akron area, are included in Ohio’s E-Check Vehicle Emissions Testing Program.
Plants as bio-indicators for ozone
