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Atmospheric methyl iodide /CH3I/It is found that atmospheric concentrations of CH3I are not greater than about 3 pptv over most of the earth's surface and drop to less than half this value above the boundary layer, suggesting that the compound is not likely to play such important roles, on a global scale, as the destruction of tropospheric O3 and free radicals and the increasing of the NO2/NO ratio and hydroxyl radical densities. It is hypothesized that a large portion of the global CH3I comes from oceanic regions of high biomass productivity, where the compound may play a key role in local atmospheric chemistry. Attention is given to CH3I measurement uncertainties with regard to global distribution, sources, and sinks.
Document ID
19820047545
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Rasmussen, R. A.
(Oregon Graduate Center for Study and Research Beaverton, OR, United States)
Khalil, M. A. K.
(Oregon Graduate Center for Study and Research Beaverton, OR, United States)
Gunawardena, R.
(Oregon Graduate Center for Study and Research Beaverton, OR, United States)
Hoyt, S. D.
(Oregon Graduate Center Beaverton, OR, United States)
Date Acquired
August 10, 2013
Publication Date
April 20, 1982
Publication Information
Publication: Journal of Geophysical Research
Volume: 87
Subject Category
Geophysics
Accession Number
82A31080
Funding Number(s)
CONTRACT_GRANT: NSF DPP-77-26380
CONTRACT_GRANT: NSG-7457
CONTRACT_GRANT: NSF ATM-78-06628
Distribution Limits
Public
Copyright
Other

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