1Laboratoire d’Optique Atmosphérique, CNRS UMR 8518, USTL, Villeneuve d’Ascq, France
2Laboratoire des Sciences du Climat et de l’Environnement, CEA/CNRS, Gif sur Yvette, France
3Laboratoire d’Océanographie Dynamique et de Climatologie, CNRS/UPMC/IRD, Paris, France
4Laboratoire de Glaciologie et Géophysique de l’Environnement, CNRS, Saint-Martin-d’Hères, France
5Max Planck Institute for Chemistry, Air Chemistry Department, Mainz, Germany
6Service d’Aéronomie, CNRS/UPMC/UVSQ, Paris, France
7Centre for Environmental Science and Engineering, Indian Institute of Technology, Bombay, India
Abstract. The global sulphur cycle has been simulated using a general circulation model with a focus on the source and oxidation of atmospheric dimethylsulphide (DMS). The sensitivity of atmospheric DMS to the oceanic DMS climatology, the parameterisation of the sea-air transfer and to the oxidant fields have been studied. The importance of additional oxidation pathways (by O3 in the gas- and aqueous-phases and by BrO in the gas phase) not incorporated in global models has also been evaluated. While three different climatologies of the oceanic DMS concentration produce rather similar global DMS fluxes to the atmosphere at 24-27 Tg S yr -1, there are large differences in the spatial and seasonal distribution. The relative contributions of OH and NO3 radicals to DMS oxidation depends critically on which oxidant fields are prescribed in the model. Oxidation by O3 appears to be significant at high latitudes in both hemispheres. Oxidation by BrO could be significant even for BrO concentrations at sub-pptv levels in the marine boundary layer. The impact of such refinements on the DMS chemistry onto the indirect radiative forcing by anthropogenic sulphate aerosols is also discussed.