Wintertime high concentration of NO
2 was analyzed by using data from air quality monitoring stations and a photochemical box model (PBM) application. The typical time variations of NO, NO
2 and O
3 during the high concentration days were clarified for sunny and cloudy day, respectively. Application of PBM was conducted by using NO
x's and NMHC's typical emission strength from Tokyo downtown area and a meteorological condition (such as temperature, humidity and mixing layer height). The relative contribution of NO2 time variation among the emission from various sources, the chemical reaction with background O
3 and the photochemical reactions were evaluated from the PBM calculation results. It was found that the oxidation of NO by the background O3 plays an important role for the concentration of NO
2 in the morning, while the contribution of the photochemical reactions becomes important in the afternoon. Also, it was concluded that the effect of photochemical reaction (oxidation of NO to NO
2) and the transformation from NO
x to PAN and HNO
3 play the significant role even in winter. These effects decrease the concentration of NO
2 in the daytime, however, these photochemically generated secondary pollutants in the daytime accelerate the increase of NO2 concentration in the evening hours.
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