BrO as a sink for dimethylsulphide in the marine atmosphere

Details BrO as a sink for dimethylsulphide in the marine atmosphere BrO as a sink for dimethylsulphide in the marine atmosphere

Jan 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994georl..21..117t&link_type=abstract

Geophysical Research Letters, Volume 21, Issue 2, p. 117-120

Physics

31

Atmospheric Composition And Structure: Biosphere/Atmosphere Interactions, Atmospheric Composition And Structure: Geochemical Cycles, Atmospheric Composition And Structure: Cloud Physics And Chemistry, Atmospheric Composition And Structure: Aerosols And Particles

Scientific paper

Dimethylsulphide (DMS) is the major biogenic sulphur source gas. It is known to be oxidized by OH and NO3 to ultimately yield sulphate particles which are important in acid deposition and are also involved in the atmospheric radiative balance. In the laboratory BrO has also been shown to oxidize DMS. Here I present atmospheric model calculations based on inorganic Bromine measurements and find that oxidation by BrO is a sink for DMS.

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