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CITY OF PLEASANTON URBAN FOREST MASTER PLAN | 139 <br />CANOPY COVER AND EQUITY <br />3.1 Why Canopy Cover Matters <br />The urban forest is an integral component of a city’s <br />infrastructure that delivers benefits every resident should <br />have equal access to. Urban forest canopy cover can <br />be inequitably distributed throughout a community and <br />different demographic groups experience wide ranges of <br />canopy cover, with sparse canopy cover often occurring <br />in socioeconomically disadvantaged and neighborhoods <br />of color. While Pleasanton doesn’t have any census tracts <br />classified as disadvantaged communities, there are several <br />neighborhoods that have less canopy cover than the City- <br />wide average of 25%. Residents in areas with lower canopy <br />cover experience fewer benefits from the urban forest, such <br />as cooler temperatures from shade, cleaner air and water, <br />access to green space, stormwater mitigation, improved <br />physical and mental health, and increased property values <br />(American Forests, 2024, Wolf 2007). <br />A City must address neighborhoods that lack tree canopy <br />cover to ensure that everyone in the community, is able to <br />experience the benefits of trees. Tree-lined streets should <br />be considered an essential aspect of providing a high quality <br />of life for residents, and it is crucial that Pleasanton continues <br />to promote the equitable distribution of its canopy cover so <br />that those tree-related benefits can be experienced by all for <br />generations to come. <br />Tree equity in Pleasanton was evaluated by assessing the <br />results of the canopy cover study against public data sources <br />and tools, including urban heat island data (Trust for Public <br />Land 2023), pollution burden data (CalEnviroScreen 2021), <br />and tree equity score (American Forests 2021). <br />3.1.1 Urban Heat Islands <br />The urban heat island (UHI) effect occurs when urban areas <br />experience higher temperatures relative to surrounding <br />non-urban areas. Multiple factors contribute to the <br />urban heat island effect, including increased impervious <br />surfaces, lack of vegetation, and increased pollutant levels. <br />Impervious surfaces, such as asphalt, concrete, buildings <br />or roofs, absorb the sun’s heat during the day, and can <br />reach temperatures that are 50°F to 90°F hotter than the <br />surrounding air temperature (EPA 2021). Lack of vegetation <br />not only limits cooling effects but also exacerbates air <br />pollution by preventing the dispersion of pollutants trapped <br />by tall buildings. The combination of increased temperatures