Methanesulfonic acid in coastal Antarctic snow related to sea-ice extent

Proxy records of biogenic sulfur gas obtained from ice cores suggest that variability in marine biogenic sulfur emissions may reflect changes in climate [Saigne and Legrand, 1987; Legrand et al., 1988, Legrand et al., 1991; Anderson and Charlson, 1991]. Increased sea‐ice extent has previously been p...

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Bibliographic Details
Published inGeophysical research letters Vol. 20; no. 6; pp. 443 - 446
Main Authors Welch, K. A., Mayewski, P. A., Whitlow, S. I.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 19.03.1993
American Geophysical Union
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Summary:Proxy records of biogenic sulfur gas obtained from ice cores suggest that variability in marine biogenic sulfur emissions may reflect changes in climate [Saigne and Legrand, 1987; Legrand et al., 1988, Legrand et al., 1991; Anderson and Charlson, 1991]. Increased sea‐ice extent has previously been proposed as one cause of relatively high methanesulfonic acid (MSA) in glacial‐age ice core samples [Gibson et al., 1990]. We have analyzed MSA, one of the oxidation products of the biogenic sulfur gas dimethylsulfide [Hatakeyama et al., 1985], from snowpit samples recovered from a coastal site in Southern Victoria Land, Antarctica. Time series of MSA correlate significantly with the longest continuous record available of Southern Ocean sea‐ice extent (two decades) [Jacka, 1990].
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ISSN:0094-8276
1944-8007
DOI:10.1029/93GL00499