Data on materials and surface types that comprise a city, i.e. urban fabric, are needed in order to estimate the effects of light-colored surfaces (roofs and pavements) and urban vegetation (trees, grass, shrubs) on the meteorology and air quality of a city. We discuss the results of a semi-automatic statistical approach used to develop data on surface-type distribution and urban-fabric makeup using aerial color orthophotography, for four metropolitan areas of Chicago, IL, Houston, TX, Sacramento, CA, and Salt Lake City, UT. The digital high resolution (0.3 to 0.5-m) aerial photographs for each of these metropolitan areas covers representative urban areas ranging from 30 km 2 to 52 km 2 .Major land-use types examined included: commercial, residential, industrial, educational, and transportation. On average, for the metropolitan areas studied, vegetation covers about 29-41% of the area, roofs 19-25%, and paved surfaces 29-39%. For the most part, trees shade streets, parking lots, grass, and sidewalks. At ground level, i.e., view from below the tree canopies, vegetation covers about 20-37% of the area, roofs 20-25%, and paved surfaces 29-36%.
IntroductionMitigating urban heat islands reduces demand for cooling-energy use and prevents smog formation (Akbari et al, 2001). In order to develop effective heat island mitigation programs, it is important to accurately characterize the urban surface, particularly in terms of surface-type distribution and vegetative fraction. An accurate characterization of the surfaces will allow a better estimate of potential increases in surface albedo 2 (roofs, pavements) and urban vegetation, providing more accurate modeling of the impact of heat-island reduction measures on ambient cooling and urban air quality.Researchers involved in the analysis of urban climate have tried to estimate the composition of various urban surfaces. In Sacramento, CA, Myrup and Morgan (1972) examined the city data in 1 Current address: Department of Geography, Florida State University, Tallahassee, Florida 32306. 2 When sunlight hits an opaque surface, some of the energy is reflected (this fraction is called albedo = a) and the rest is absorbed (the absorbed fraction is 1-a). Low-a surfaces become much hotter than high-a surfaces.Submitted to Journal of the Human-Environment System 2 progressively smaller integral segments of macro-scale (representative areas of Sacramento), mesoscale (individual communities), micro-scale (land-use ordinance zones), and basic-scale (city blocks).The data used included the United States Geological Survey (USGS) photos, parks and recreation plans, city engineering roadways, and detailed aerial photos. The analysis covered 195 km 2 of the urban area. The calculated percentages of the land-use areas are as follows: residential 35.5%, commercial 7.2%, industrial 13.5%, streets and freeways 17.0%, institutional 3.2%, and open space and recreational 23.6%. The analysis found the average residential area to be about 22% streets, 23%roofs, 22% other impervious surfaces, ...