Abstract
The extent to which ozone has been decreasing over the past two decades has been reported by many researchers and the results have been summarized in periodic international scientific assessments on ozone depletion (e.g. WMO, 1991; 1994). These assessments have quantified the long-term trends in ozone as functions of latitude and time of year and have summarized findings which associate these changes to enhanced levels of stratospheric chlorine and bromine that are anthropogenic in origin. The long-term trend values are based on the results of analyses of stratospheric ozone measurements which have been made routinely on a global scale for nearly four decades.
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Kerr, J.B. (1998). The Evolving Uv Climate. In: Le Prestre, P.G., Reid, J.D., Morehouse, E.T. (eds) Protecting the Ozone Layer. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-5585-8_4
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DOI: https://doi.org/10.1007/978-1-4615-5585-8_4
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