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Tropospheric chemistryThe chemistry of the background troposphere, the source region, and the transition regions are discussed. The troposphere is governed by heterogeneous chemistry far more so than the stratosphere. Heterogeneous processes of interest involve scavenging of trace gases by aerosols, cloud and precipitation elements leading to aqueous phase chemical reactions and to temporary and permanent removal of material from the gas phase. Dry deposition is a major removal process for ozone, as well as for other gases of importance in tropospheric photochemistry. These processes are also discussed.
Document ID
19870001182
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Mohnen, V. A.
(NASA Headquarters Washington, DC United States)
Chameides, W.
(NASA Headquarters Washington, DC United States)
Demerjian, K. L.
(NASA Headquarters Washington, DC United States)
Lenschow, D. H.
(NASA Headquarters Washington, DC United States)
Logan, J. A.
(NASA Headquarters Washington, DC United States)
Mcneal, R. J.
(NASA Headquarters Washington, DC United States)
Penkett, S. A.
(NASA Headquarters Washington, DC United States)
Platt, U.
(NASA Headquarters Washington, DC United States)
Schurath, U.
(NASA Headquarters Washington, DC United States)
Dias, P. D.
(NASA Headquarters Washington, DC United States)
Date Acquired
August 13, 2013
Publication Date
January 1, 1985
Publication Information
Publication: Atmospheric Ozone 1985. Assessment of our Understanding of the Processes Controlling its Present Distribution and Change, Volume 1
Subject Category
Geophysics
Accession Number
87N10615
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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