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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Published in | Environmental monitoring and assessment Vol. 196; no. 7; p. 658 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Cham
Springer International Publishing
01.07.2024
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0167-6369 1573-2959 1573-2959 |
DOI: | 10.1007/s10661-024-12830-9 |