2011
DOI: 10.1016/j.proenv.2011.03.017
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Influence of meteorological conditions on summer ozone levels in the central Kanto area of Japan

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Cited by 47 publications
(27 citation statements)
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“…Urban forest forms a microclimate that differs from that of an urban environment because of its ecological characteristics such as its large canopy cover, the special underlying surface, and the physiological activities of plants [71][72][73]. Microclimate parameters such as air temperature, relative humidity, wind speed, and solar radiation may play an important role in the formation, dispersion, and transport of O 3 [74][75][76].…”
Section: Impact Of Micrometeorological Parameters On O 3 Levelsmentioning
confidence: 99%
“…Urban forest forms a microclimate that differs from that of an urban environment because of its ecological characteristics such as its large canopy cover, the special underlying surface, and the physiological activities of plants [71][72][73]. Microclimate parameters such as air temperature, relative humidity, wind speed, and solar radiation may play an important role in the formation, dispersion, and transport of O 3 [74][75][76].…”
Section: Impact Of Micrometeorological Parameters On O 3 Levelsmentioning
confidence: 99%
“…Our result is not a rare event. In fact, while vigorous O 3 formation in the summer (high levels of solar irradiance and abundant O 3 precursor concentrations) has long been recognized by several authors, high levels of O 3 production during the winter has only recently been documented (Kalabokas et al, 2013;Ooka et al, 2011). The strong role of meteorology (thermic inversion), topography, and high levels of O 3 precursors from oil refinery activities (with high density in Tabriz) in association to home heating and vehicle traffic have been identified as key drivers of wintertime high O 3 events.…”
Section: Discussionmentioning
confidence: 99%
“…Nitrogen dioxide and volatile organic compounds (i.e., primary pollutants) in presence of stagnant high‐pressure, strong solar radiation, and high air temperature—typical features of UHI—trigger complex chemical reactions which give rise to O 3 formation (Stone, ) (i.e., a secondary pollutant) and limit its dissipation (Li, Song, Mao, Liu, & Huang, ; Ooka et al., ). Although O 3 formation follows complex and nonlinear dynamics—to which contribute numerous factors like the concentration of its precursors, humidity, and solar intensity (Comrie, )—high temperature is a key driver because it accelerates its generation (Tao, Larson, Wuebbles, Williams, & Caughey, , ).…”
Section: Uhi and Lca Methodologymentioning
confidence: 99%