4.7 Article

Ambient ozone at a rural Central European site and its vertical concentration gradient close to the ground

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 30, Issue 33, Pages 80014-80028

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-023-28016-8

Keywords

Ground-level ozone; Vertical profile; Czech Republic; Kosetice; 2015-2021; GAM

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This study aims to explore the vertical distribution of ground-level ozone concentrations and examine the O-3 concentration gradients at different heights. Daily mean O-3 concentrations measured at the Kosetice station during 2015-2021 are analyzed using the GAM approach. The study finds significant variations in the O-3 concentration gradients at different height ranges, with the highest dynamics observed between 2 and 8 meters and differences in seasonal and annual aspects.
The representativeness of ambient air quality of an in situ measurement is key in the use and correct interpretation of the measured concentration values. Though the horizontal representativeness aspect is generally not neglected in air pollution studies, a detailed, high-resolution vertical distribution of ambient air pollutant concentrations is rarely addressed. The aim of this study is twofold: (i) to explore the vertical distribution of ground-level ozone (O-3) concentrations measured at four heights above the ground-namely at 2, 8, 50, and 230 m-and (ii) to examine in detail the vertical O-3 concentration gradient in air columns between 2 and 8, 8 and 50, and 50 and 230 m above the ground. We use the daily mean O-3 concentrations measured continuously at the Kosetice station, representing the rural Central European background ambient air quality observed during 2015-2021. We use the semiparametric GAM (generalised additive model) approach (with complexity or roughness-penalised splines implementation) to analyse the data with sufficient flexibility. Our models for both O-3 concentrations and O-3 gradients use (additive) decomposition into annual trend and seasonality (plus an overall intercept). The seasonal and year-to-year patterns of the modelled O-3 concentrations look very similar at first glance. Nevertheless, a more detailed look through O-3 gradients shows that they differ substantially with respect to their seasonal and long-term dynamics. The vertical O-3 concentration gradient in 2-230 m is not uniform but changes substantially with increasing height and shows by far the highest dynamics near the ground between 2 and 8 m, differing in both the seasonal and annual aspects for all the air columns inspected. We speculate that non-linear changes of both seasonal and annual components of vertical O-3 gradients are due to atmospheric-terrestrial interactions and to meteorological factors, which we will explore in a future study.

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