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Sulfur isotope measurements of submicrometer sulfate aerosol particles over the Pacific Ocean
Author(s) -
Calhoun Julie A.,
Bates Timothy S.,
Charlson Robert J.
Publication year - 1991
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/91gl02304
Subject(s) - sulfate , seawater , aerosol , sulfur , sulfate aerosol , environmental chemistry , fractionation , isotope fractionation , sulfur cycle , atmosphere (unit) , sea salt , environmental science , geology , oceanography , meteorology , chemistry , organic chemistry , physics
The climatic importance of atmospheric submicrometer sulfate aerosol particles necessitates a thorough understanding of the various sources of sulfur to the marine atmosphere [Charlson et al., 1987; Coakley et al., 1987; Charlson et al., 1990]. Over the remote ocean, the primary source of atmospheric non‐seasalt (NSS) sulfate is thought to be marine emissions of dimethylsulfide (DMS) [Charlson et al., 1987]. Here we report the results of a study which used stable sulfur isotopes to test this hypothesis. NSS sulfate in submicrometer aerosol particles over remote parts of the South Pacific Ocean had an average δ 34 S value of +15.6±3.1‰, relative to the Canyon Diablo standard. The sulfur isotopic composition of these particles was 5.5‰ lighter than sulfate derived directly from seawater, but isotopically heavier than sulfate derived from most continental sources. This observed isotopic fractionation between seawater sulfate and NSS sulfate is consistent with the isotopic fractionation predicted for the transformation of seawater sulfate to atmospheric NSS sulfate via a DMS pathway (−1 to +7‰) and hence supports the hypothesis that DMS can be the source of the NSS sulfate.