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Ultraviolet radiation changesA major consequence of ozone depletion is an increase in solar ultraviolet (UV) radiation received at the Earth's surface. This chapter discusses advances that were made since the previous assessment (World Meteorological Organization (WMO)) to our understanding of UV radiation. The impacts of these changes in UV on the biosphere are not included, because they are discussed in the effects assessment.
Document ID
19930001910
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Mckenzie, Richard L. (Department of Scientific and Industrial Research Lauder, New Zealand)
Frederick, John E. (Illinois Univ. Chicago., United States)
Ilyas, Mohammad (Sains Malaysia Univ. Penang., United States)
Filyushkin, V. (Central Aerological Observatory Dolgoprudnyi, Ussr)
Wahner, Andreas (Kernforschungsanlage Juelich, Germany)
Stamnes, K. (Alaska Univ. Fairbanks., United States)
Muthusubramanian, P. (Madurai-Kamaraj Univ. Madurai, India)
Blumthaler, M. (Innsbruck Univ. Austria)
Roy, Colin E. (Australian Radiation Lab. Melbourne., United States)
Madronich, Sasha (National Center for Atmospheric Research Boulder, CO., United States)
Date Acquired
September 6, 2013
Publication Date
January 1, 1991
Publication Information
Publication: NASA, Washington, Scientific Assessment of Ozone Depletion: 1991
Subject Category
Environment Pollution
Accession Number
93N11098
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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IDRelationTitle19930001899Collected WorksScientific assessment of ozone depletion: 1991
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