
Francisco Escobedo, Jennifer A. Seitz, and Wayne Zipperer2
Poor air quality is a common problem in many urban areas. It can lead to human health problems and reduced visibility, and it can impair the health of plants and wildlife. The urban forest can help improve air quality by removing pollutants and by reducing air temperature through shading and transpiration. Trees also emit volatile organic compounds that can indirectly contribute to ozone formation. The USDA Forest Service's Urban Forest Effects (UFORE) Model was used to better understand air pollution removal by urban trees in Gainesville, Florida.
A tree is able to remove air pollution via its leaves in two ways. The first is by direct uptake through the leaf stomata. Once inside the leaf, gases diffuse into intercellular spaces. There they may be absorbed by water films to form acids or they may react with the surfaces of the inner-leaf. The second way leaves remove air pollution is by intercepting and retaining particles on the leaf surfaces. The intercepted particle often is re-suspended to the atmosphere by wind, washed off by rain, or deposited on the ground through leaf fall (Escobedo 2007).
Pollution removal by trees in Gainesville was estimated using field data from 93 sites and hourly pollution and weather data for 2000. The amount of pollution removal was calculated for ozone (O3), sulfur dioxide (SO2), nitrogen dioxide (NO2), carbon monoxide (CO), and particulate matter less than ten microns (PM10).
An average square meter of tree cover in Gainesville removes 6 grams of air pollutants in one year. Total pollution removal was greatest for ozone, followed by particulate matter less than ten microns, sulfur dioxide, nitrogen dioxide, and carbon monoxide. Figure 1 compares pollution removal for different pollutants and shows the economic benefits of pollution removal to society (pollution removal reduces health care costs because people breathe fewer harmful pollutants). It is estimated that in 2000 trees removed 390 metric tons of air pollution (CO, NO2, O3, PM10, SO2) per year. This translated to around $2 million in economic benefits.
Trees can also reduce temperature for a given area based on the amount of tree density and cover. Figure 2 demonstrates how increased trees in forests and forested vacant areas help reduce temperatures as opposed to transportation areas and parks and institutions with little tree cover. Shading and transpiration from trees can affect the overall microclimate of an area by modifying ambient temperature and solar radiation. In most cases transpiration and shading from trees reduce summertime temperatures, which may reduce the amount of energy used to cool buildings.
Comparison of the pollutants removed by the City of Gainesville's urban forests, by metric tons removed and by health care dollars saved. Escobedo and Zipperer. 2007.
Temperature reduction due to tree cover in Gainesville, Florida's seven land use areas. Escobedo and Zipperer. 2007.
When vegetation is limited in a community, researchers have found that buildings and paved surfaces absorb energy from the sun, causing the surface temperature of urban structures to become 10–21°C (18–38°F) higher than the ambient air temperatures (Taha and others 1992). As the surfaces become hotter, the overall ambient air temperature also increases, resulting in a phenomenon, known as an "urban heat island." Urban heat islands can raise air temperature in a city by 1.1–4.5°C (1–8°F) (World Meteorological Organization 1984).
The urban heat island effect is caused by buildings, sidewalks, paved roads, and other non-natural surfaces that limit the amount of land covered with vegetation like grass and trees. Land surfaces with vegetation offer high moisture levels that cool the air when the moisture evaporates from soil and plants. Often a community has fewer vegetated areas and more water-resistant surfaces such as asphalt and building materials that absorb most of the sun's radiation. These surfaces hinder the natural cooling that would otherwise take effect with the evaporation of moisture from surfaces with vegetation.
The higher temperatures in urban heat islands increase air conditioning and can raise pollution levels. Natural compounds called volatile organic compounds are produced from certain trees in high temperatures during the summer. These compounds react with existing pollution under certain climatic conditions to form smog. Through shade provided by trees, ambient temperatures can be reduced, thus lowering the likelihood of smog being formed.
The function of the urban forest is dependent on its structure, cover, and urban morphology (For more information on these topics read the Gainesville Urban Forest Fact Sheet Series). Trees provide an important ecosystem service by helping to reduce air pollution and temperature. Land managers can take steps to maintain and improve air quality and reduce the demand for energy in cooling by following these management strategies:
Increase the number of healthy trees to increase pollution removal.
Plant trees on the west side of buildings to help shade during the hottest part of the day.
Sustain existing tree cover to maintain pollution removal levels and provide shade.
Sustain large, healthy trees since they have greatest per-tree effects.
Use long-lived trees since they reduce long-term pollutant emissions from planting and removal.
Use low-maintenance trees to reduce pollutant emissions from maintenance activities.
Plant trees in polluted or heavily populated areas to maximize tree air quality benefits.
Use pine and evergreen hardwood trees for particulate matter reduction since they keep their needles and leaves all year for year-round removal of particles.
Escobedo, F. 2007. Urban Forests in Florida: Do they reduce air pollution? (FOR 128). Gainesville FL: School of Forest Resources and Conservation, Florida Cooperative Extension Service, Institute of Food and Agricultural Sciences, University of Florida.
Escobedo, F. and W. Zipperer. 2007. Assessing Gainesville's urban forest effects and values. Unpublished raw data.
Taha, H., D. Sailor, and H. Akbari. 1992. High-albedo Materials for Reducing Building Cooling Energy Use. Lawrence Berkeley National Laboratory Report No. 31721 UC-350: 71.
World Meteorological Organization. 1984. "Urban Climatology and its Applications with Special Regard to Tropical Areas." Proceedings of the Technical Conference Organized by The World Meteorological Organization, Mexico, 26-30 November 1984 (WMO-No. 652): 534.
This document is FOR216, one of a series of the School of Forest Resources and Conservation Department, Florida Cooperative Extension Service, Institute of Food and Agricultural Sciences, University of Florida. Original publication date May 6, 2009. Visit the EDIS Web site at http://edis.ifas.ufl.edu.
Francisco Escobedo, assistant professor, Jennifer A. Seitz, Extension associate, School of Forest Resources and Conservation, Institute of Food and Agricultural Sciences, University Florida. Wayne Zipperer, research scientist, USDA Forest Service.
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