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Photochemistry of tropospheric ozoneA photochemical equilibrium model of minor constituent chemistry in the troposphere was constructed to investigate the photochemistry of tropospheric ozone. We find that photochemical production must be supplemented by additional sources to account for observed ozone levels in clean air, while photochemical loss is more important than surface destruction as an ozone loss mechanism. Photochemically produced ozone is sensitive to the NO(x) background in the model, exhibiting a maximum of about 0.5 ppb of NO(x).
Document ID
19770059294
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Stewart, R. W. (NASA Goddard Institute for Space Studies New York, N.Y., United States)
Hameed, S. (NASA Goddard Inst. for Space Studies New York, NY, United States)
Pinto, J. P. (New York, State University Stony Brook, N.Y., United States)
Date Acquired
August 9, 2013
Publication Date
July 20, 1977
Publication Information
Publication: Journal of Geophysical Research
Volume: 82
Subject Category
Geophysics
Accession Number
77A42146
Funding Number(s)
CONTRACT_GRANT: NSG-5102
Distribution Limits
Public
Copyright
Other

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