Abstract
Through the production of highly reactive hydroxyl radicals by photolysis of ozone in ultraviolet solar radiation, ozone is one of the most important gases in the troposphere. The hydroxyl radicals which are present only at very low concentrations in the troposphere (global average about 5×105 molecules cm-3) attack virtually all hydrogen containing gases that are emitted into the atmosphere by both natural processes and anthropogenic activities and in addition such important gases as CO, NO2 and SO2. It is clear that tropospheric ozone is an essential compound in the atmospheric environment.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1988 D. Reidel Publishing Company
About this chapter
Cite this chapter
Crutzen, P. et al. (1988). Background Ozone. In: Isaksen, I.S.A. (eds) Tropospheric Ozone. NATO ASI Series, vol 227. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-2913-5_27
Download citation
DOI: https://doi.org/10.1007/978-94-009-2913-5_27
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-7811-5
Online ISBN: 978-94-009-2913-5
eBook Packages: Springer Book Archive