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contributor authorMcElroy, Michael B.
contributor authorDak Sze, Nien
contributor authorLing Yung, Yuk
date accessioned2017-06-09T14:17:12Z
date available2017-06-09T14:17:12Z
date copyright1973/10/01
date issued1973
identifier issn0022-4928
identifier otherams-16453.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152238
description abstractCarbon monoxide, produced in the Venus atmosphere by photolysis of CO2, is removed mainly by reaction with OH. The radical OH is formed in part by photolysis of H2O2, in part by reaction of 0 with H02. Photolysis of HCl provides a major source of H radicals near the visible clouds of Venus and plays a major role in the overall photochemistry. The mixing ratio of 02 is estimated to be approximately 10?7, about a factor of 10 less than a recent observational upper limit reported by Traub and Carleton. A detailed model, which accounts for the photochemical stability of Venus CO2, is presented and discussed.
publisherAmerican Meteorological Society
titlePhotochemistry of the Venus Atmosphere
typeJournal Paper
journal volume30
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1973)030<1437:POTVA>2.0.CO;2
journal fristpage1437
journal lastpage1447
treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007
contenttypeFulltext


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