Characteristics of surface ozone pollution and its correlations with meteorological factors: the case of Xiangtan

Based on ozone (O 3 ) monitoring data for Xiangtan and meteorological observation data for 2020–2022, we examined ozone pollution characteristics and the effects of meteorological factors on daily maximum 8-h average ozone (O 3-8h ) concentrations in Xiangtan. Thus, we observed significant increases...

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Bibliographic Details
Published inEnvironmental monitoring and assessment Vol. 196; no. 7; p. 658
Main Authors Lizhi, He, Zhenghui, Xiao, Cheng, Xie, Yongquan, Long
Format Journal Article
LanguageEnglish
Published Cham Springer International Publishing 01.07.2024
Springer Nature B.V
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Summary:Based on ozone (O 3 ) monitoring data for Xiangtan and meteorological observation data for 2020–2022, we examined ozone pollution characteristics and the effects of meteorological factors on daily maximum 8-h average ozone (O 3-8h ) concentrations in Xiangtan. Thus, we observed significant increases as well as notable seasonal variations in O 3-8h concentrations in Xiangtan during the period considered. The ozone and temperature change response slope ( K O3-T ) indicated that local emissions had no significant effect on O 3-8h generation. Further, average O 3-8h concentration and maximum temperature ( T max ) values showed a polynomial distribution. Specifically, at T max < 27 °C, it increased almost linearly with increasing temperature, and at T max between 27 and 37 °C, it showed an upward curvilinear trend as temperature increased, but at a much lower rate. Then, at T max > 37 °C, it decreased with increasing temperature. With respect to relative humidity (RH), the average O 3-8h concentration primarily exceeded the standard value when RH varied in the range of 45–65%, which is the key humidity range for O 3 pollution, and the inflection point for the correlation curve between O 3-8h concentration and RH appeared at ~55%. Furthermore, at wind speeds (WSs) below 1.5 m∙s −1 , O 3-8h concentration increased rapidly, and at WSs in the 1.5–2 m∙s −1 range, it increased at a much faster rate. However, at WSs > 2 m∙s −1 , it decreased slowly with increasing WS. O 3-8h concentration also showed the tendency to exceed the standard value when the dominant wind directions in Xiangtan were easterly or southeasterly.
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ISSN:0167-6369
1573-2959
1573-2959
DOI:10.1007/s10661-024-12830-9