Abstract
Vegetation canopies are efficient in removing ozone (O3) from the atmosphere making surface dry deposition an important process in air quality but also in climate change. O3 is the 3rd most important greenhouse gas (IPCC) responsible for ~25 % of the total net radiative forcing attributed to human activities.
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Ganzeveld, L., Ammann, C., Loubet, B. (2015). Modelling Atmosphere-Biosphere Exchange of Ozone and Nitrogen Oxides. In: Massad, RS., Loubet, B. (eds) Review and Integration of Biosphere-Atmosphere Modelling of Reactive Trace Gases and Volatile Aerosols. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-7285-3_3
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