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Vertical ozone formation mechanisms driven by deep convection within the boundary layer over the Loess Plateau, China
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DOI：10.1016/j.envres.2026.125454.png)
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Abstract
En 中文
• Vertical distribution of VOCs in the boundary layer over the Loess Plateau was clarified. • Contributions of residual layer input and photochemical formation to ozone were quantified. • Strong convection leads to NOx accumulation in the upper atmosphere, rendering the entire boundary layer a VOCs-controlled region.
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7.7
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2.0W
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9.0W
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