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Measurements of solar ultraviolet radiation and atmospheric photolysis rates

Journal Article · · Atmos. Technol.; (United States)
OSTI ID:6300977

Ozone in the upper atmosphere controls how much of the sun's ultraviolet (uv) radiation reaches the earth. Ozone (O/sub 3/) is produced through the photolysis of oxygen. Ozone is itself photolyzed by the sun to form excited oxygen atoms which can react with nitrous oxide (N/sub 2/O) to form nitric oxide (NO); NO, in turn, exerts a controlling influence on stratospheric ozone. Solar photolysis reactions are also the keystone of photochemical smog formation. Most of the ozone in the polluted troposphere is derived from the photolysis of nitrogen dioxide (NO/sub 2/). Tropospheric photolysis reactions run the spectrum from the shortest ultraviolet to the longest visible radiation. This article describes new experimental techniques for measuring the intensity of photolyzing radiation throughout the troposphere.

OSTI ID:
6300977
Journal Information:
Atmos. Technol.; (United States), Journal Name: Atmos. Technol.; (United States) Vol. 12; ISSN ATTED
Country of Publication:
United States
Language:
English