Seasonal variations of atmospheric sulfur dioxide and dimethylsulfide concentrations at Amsterdam Island in the southern Indian Ocean

Daily measurements of atmospheric sulfur dioxide (SO2) concentrations were performed from March 1989 to January 1991 at Amsterdam Island (37°50′ S–77°30′ E), a remote site located in the southern Indian Ocean. Long-range transport of continental air masses was studied using Radon (222Rn) as continental tracer. Average monthly SO2 concentrations range from less than 0.2 to 3.9 nmol m-3 (annual average = 0.7 nmol m-3) and present a seasonal cycle with a minimum in winter and a maximum in summer, similar to that described for atmospheric DMS concentrations measured during the same period. Clear diel correlation between atmospheric DMS and SO2 concentrations is also observed during summer. A photochemical box model using measured atmospheric DMS concentrations as input data reproduces the seasonal variations in the measured atmospheric SO2 concentrations within ±30%. Comparing between computed and measured SO2 concentrations allowed us to estimate a yield of SO2 from DMS oxidation of about 70%.

[1]  M. Andreae,et al.  Airborne measurements of dimethylsulfide, sulfur dioxide, and aerosol ions over the Southern Ocean South of Australia , 1990 .

[2]  R. Jenne,et al.  Atlas of Simultaneous Occurrence of Different Cloud Types Over the Ocean , 1982 .

[3]  C. J. Hahn,et al.  The biogeochemical sulfur cycle in the marine boundary layer over the Northeast Pacific Ocean , 1990 .

[4]  P. Wine,et al.  Kinetics and mechanism of hydroxyl reactions with organic sulfides , 1986 .

[5]  P. W. West,et al.  Fixation of Sulfur Dioxide as Disulfitomercurate (II) and Subsequent Colorimetric Estimation , 1956 .

[6]  W. Jaeschke,et al.  Measurements of H2S and SO2 over the Atlantic Ocean , 1984 .

[7]  J. Servant,et al.  The origins of sulfur compounds in the atmosphere of a zone of high productivity (Gulf of Guinea) , 1982 .

[8]  I. Barnes,et al.  FTIR study of the DMS/NO2/I2/N2 photolysis system: the reaction of IO radicals with DMS , 1987 .

[9]  H. Rodhe,et al.  On the relation between anthropogenic SO2 emissions and concentration of sulfate in air and precipitation , 1989 .

[10]  R. W. Gillett,et al.  Coherence between seasonal cycles of dimethyl sulphide, methanesulphonate and sulphate in marine air , 1991, Nature.

[11]  H. Berresheim Biogenic sulfur emissions from the Subantarctic and Antarctic Oceans , 1987 .

[12]  J. Prospero,et al.  Methane sulfonic acid in the marine atmosphere , 1983 .

[13]  G. Lambert,et al.  Residence time of sulfur dioxide in the marine atmosphere , 1975 .

[14]  J. Gras Baseline atmospheric condensation nuclei at Cape Grim 1977–1987 , 1990 .

[15]  A. Guenther,et al.  Sulfur emissions to the atmosphere from natural sourees , 1992 .

[16]  R. A. Cox,et al.  Evaluated kinetic and photochemical data for atmospheric chemistry: Supplement II , 1989 .

[17]  T. Bates,et al.  Vertical distribution of dimethylsulfide, sulfur dioxide, aerosol ions, and radon over the Northeast Pacific Ocean , 1988 .

[18]  M. Kritz Exchange of sulfur between the free troposphere, marine boundary layer, and the sea surface , 1982 .

[19]  P. D. Houmere,et al.  Correction [to “Dimethyl sulfide in the marine atmosphere” by M. O. Andreae, R. J. Ferek, F. Bermond, K. P. Byrd, R. T. Engstrom, S. Hardin, P. D. Houmere, F. LeMarrec, H. Raemdonck, and R. B. Chatfield] , 1986 .

[20]  T. Bates,et al.  Regional and seasonal variations in the flux of oceanic dimethylsulfide to the atmosphere , 1987 .

[21]  P. Crutzen,et al.  Scale problems in global tropospheric chemistry modeling: Comparison of results obtained with a three-dimensional model, adopting longitudinally uniform and varying emissions of NOX and NMHC , 1993 .

[22]  J. Galloway,et al.  A study of the sulfur cycle in the Antarctic marine boundary layer , 1989 .

[23]  Retrieval of microphysical variables by a diagnostic modelling study: comparison between parameterized and detailed warm microphysics , 1989 .

[24]  Jin Wu Roughness elements of the sea surface—their spectral composition , 1986 .

[25]  S. Warren,et al.  Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate , 1987, Nature.

[26]  J. Gras Cloud condensation nuclei over the Southern Ocean , 1990 .

[27]  Henning Rodhe,et al.  A global three-dimensional model of the tropospheric sulfur cycle , 1991 .

[28]  Ian Barnes,et al.  Kinetics and mechanisms of the reaction of OH radicals with dimethyl sulfide , 1988 .

[29]  G. Lambert,et al.  The atmospheric concentration of sulfure dioxide and sulfate aerosols over antarctic, subantarctic areas and oceans , 1974 .

[30]  G. Lambert,et al.  Sulfate enrichment in marine aerosols owing to biogenic gaseous sulfur compounds , 1980 .

[31]  P. Liss,et al.  The seasonal variation of dimethyl sulfide and dimethylsulfoniopropionate concentrations in nearshore waters1 , 1988 .

[32]  G. Lambert,et al.  Long-range transport of continental radon in subantarctic and antarctic areas , 1986 .

[33]  N. Mihalopoulos,et al.  Seasonal variation of atmospheric dimethylsulfide at Amsterdam Island in the southern Indian Ocean , 1990 .

[34]  Paul J. Crutzen,et al.  The role of clouds in tropospheric photochemistry , 1991 .

[35]  J. Galloway,et al.  Sulfur dioxide over the western North Atlantic Ocean during GCE/CASE/WATOX , 1990 .

[36]  J. Seinfeld,et al.  Analysis of atmospheric photooxidation mechanisms for organosulfur compounds , 1986 .

[37]  P. D. Houmere,et al.  Dimethyl sulfide in the marine atmosphere , 1985 .

[38]  H. Sievering,et al.  Sulfur dry deposition over the western North Atlantic: the role of coarse aerosol particles , 1989 .

[39]  B. Bonsang,et al.  The role of the ocean in the global atmospheric sulfur cycle , 1983 .