Ozone is not emitted directly from any man-made source in any significant quantities. In the lower atmosphere, ozone is primarily formed by a complicated series of chemical reactions initiated by sunlight. These reactions can be summarised as the sunlight-initiated oxidation of volatile organic compounds (VOCs) in the presence of nitrogen oxides (NOx). The sources of VOCs are similar to those described for NOx above, but also include other activities such as solvent use, and petrol distribution and handling.
The chemical reactions do not take place instantaneously, but can take hours or days, therefore ozone measured at a particular location may have arisen from VOC and NOx emissions many hundreds or even thousands of miles away and is therefore known as ‘trans boundary’.
The objective level for ozone is set as a 8 hour mean however this is not currently included in Scottish Regulations and therefore is not routinely monitored by Local Government Authorities, including Dundee City Council.
Ozone in high concentrations can cause irritation to the eyes and the airways of the lungs and increasing the symptoms of those suffering from asthma and lung diseases. At very high concentrations ozone can damage airways leading to inflammatory reactions. There is also a potential for ozone to damage ecosystems.