Investigating ozone build-up in the east of England during the July 2015 heat wave
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2025
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Source Science of The Total Environment, 979, 179464
Details
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Journal Title:Science of The Total Environment
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Personal Author:
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NOAA Program & Office:
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Description:Ozone (O₃) precursors controls have reduced peak episodes in the UK, yet some regions still exceed the 50 ppbv (8-h) limit under certain meteorological conditions. This study uses O₃-tagging within WRF-Chem to quantify NOₓ contributions to near-surface O₃ across the East of England during a short heatwave (30 June-5 July 2015), where O₃ peaked at 116 ppbv. Despite underestimating peak O₃, the model effectively captures the episode's evolution and spatial extent (MB: −2 ppbv, r: 0.78), depicting O₃ increases on the hottest days and their decline. During the peak O₃ event, Western Europe contributed ∼60 % of daily mean O₃, while domestic NOₓ emissions accounted for only ∼4.6 %. South-easterly winds transported O₃ and precursors from BENELUX, France, Germany, the North Sea, and the English Channel. Near-surface wind convergence (−0.00002 s −1) with weaker westerlies redirected domestic O₃ to the central UK, intensifying continental influence. Conversely, south-south-westerly flows amplified domestic O₃ contributions. Analysis of the processes contributing to O₃ build-up highlights that transboundary transport played a significant role during the peak event. Boundary layer growth contributed by entraining O₃-rich air (up to 10.3 ppb h −1 across the boundary layer top), along with precursors from the residual layer, facilitating their downward mixing to surface levels. This process set the stage for in-situ photochemical O₃ production, which peaked at midday, contributing to a total daily O₃ production of 42 ppbv on average across the region. Our findings underscore the necessity of coordinated international efforts to manage transboundary pollution, alongside targeted local measures to reduce O₃ precursor emissions. O₃-tagging in WRF-Chem quantifies NOₓ contributions to the observed O₃ build-up SE winds brought O₃ from Western EU (60 %), while UK NOₓ contributed 4.6 % Domestic sources had a greater impact on surface O₃ during south-southwesterly flows
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Source:Science of The Total Environment, 979, 179464
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DOI:
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ISSN:0048-9697
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Pubmed ID:40267651
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Rights Information:CC BY-NC
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Compliance:Library
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Main Document Checksum:urn:sha-512:c65bcd4958717818b937facf520e87cd3a01c3e3d77b13a69b3a8155630af58a0c69201283c771c11953b830a6a7e56064fc7b06b3906f8e7251eafa577388ae
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