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Tropospheric Ozone Budget: Formation, Depletion and Climate Change

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Tropospheric Ozone and its Impacts on Crop Plants

Abstract

Because tropospheric O3 is a secondary pollutant, its concentration in the troposphere largely depends upon different variables that play major roles in its in-situ production. Formation of O3 in the troposphere largely depends upon the emission of it’s precursors like nitrogen oxides (NOx) and volatile organic compounds (VOCs) along with a set of favourable meteorological conditions such as high temperature, intense solar radiations, long sunshine hours, wind speed/direction, etc. In addition, tropospheric O3 concentration also depends upon the stratospheric intrusion which shows significant seasonal and zonal variations. Apart from O3 formation, the O3 budget in the troposphere is also determined by O3 destruction/depletion, which is more prominent in marine boundary layer, characterized by the production of halogen species like chlorine (Cl), bromine (Br) and iodine (I) and their respective oxides. This chapter emphasizes the role of different factors determining O3 formation/depletion and the conditions which significantly affect the tropospheric O3 budget. The effect of climate change variables on tropospheric O3 budget is also discussed.

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  1. Department of Botany, Institute of Science, Banaras Hindu University, Varanasi, UP, India

    Supriya Tiwari & Madhoolika Agrawal

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Tiwari, S., Agrawal, M. (2018). Tropospheric Ozone Budget: Formation, Depletion and Climate Change. In: Tropospheric Ozone and its Impacts on Crop Plants. Springer, Cham. https://doi.org/10.1007/978-3-319-71873-6_2

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