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IMPACT OF OCEANIC SOURCES OF BIOGENIC SULFUR ON SULFATE AEROSOL CONCENTRATIONS AT MAWSON, ANTARCTICA
Author(s): PROSPERO JM, SAVOIE DL, SALTZMAN ES, LARSEN R
Source: NATURE    Volume: 350    Issue: 6315    Pages: 221-223    Published: MAR 21 1991  
Times Cited: 86     References: 28     
Abstract: Sulphate is the dominant aerosol species in the Antarctic atmosphere 1,2 and an important constituent in Antarctic snow and ice 3. Various sources have been suggested for Antarctic non-sea-salt sulphate (n.s.s. SO4(2-)): volcanic emissions, stratospheric injection, pollutants transported from the low latitudes and biogenic dimethylsulphide (DMS) from the ocean 1,2. Although the oceanic source is now believed to be especially important, there has been no strong chemical evidence directly linking oceanic DMS with the Antarctic n.s.s. SO4(2-) concentrations. Here we present extended measurements from the Antarctic for both n.s.s. SO4(2-) and methanesulphonate (MSA), an oxidation product of DMS. Both species have a very strong seasonal cycle with a maximum in the austral summer; this cycle parallels that of the oceanic biogenic sulphur producers, thereby suggesting a strong link between the Antarctic atmospheric sulphur cycle and biological processes in the Southern Ocean.
Document Type: Article
Language: English
Reprint Address: PROSPERO, JM (reprint author), UNIV MIAMI, ROSENSTIEL SCH MARINE & ATMOSPHER SCI, MAC, 4600 RICKENBACKER CAUSEWAY, MIAMI, FL 33149 USA
Addresses:
1. US DOE, ENVIRONM MEASUREMENTS LAB, NEW YORK, NY 10014 USA
Publisher: MACMILLAN MAGAZINES LTD, 4 LITTLE ESSEX STREET, LONDON, ENGLAND WC2R 3LF
Subject Category: Multidisciplinary Sciences
IDS Number: FC779
ISSN: 0028-0836
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