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Sources of SO and SO 2 in the Mesosphere of Venus Yuk L. Yung, X. Zhang, M. C. Liang, F. P. Mills, D. A. Belyaev Caltech EPSC-DPS 2011, NANTES, FRANCE. Belyaev et al. (2011). Zhang et al. (2011). SO ( H 2 SO 4 Case ). SO 2 ( H 2 SO 4 Case ). SO 3 ( H 2 SO 4 Case ).
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Sources of SO and SO2 in the Mesosphere of Venus Yuk L. Yung, X. Zhang, M. C. Liang, F. P. Mills, D. A. Belyaev Caltech EPSC-DPS 2011, NANTES, FRANCE
Conclusion • A sulfur source is required to explain the SO2 inversion layer above 80 km. • The evaporation of the aerosols composed of sulfuric acid or polysulfurabove 90 km could provide the sulfur source. • Measurements of SO3 and SO (a1∆→X3∑) emission at 1.7 μm may be the key to distinguish between the two models.
Acknowledgement • NASA Grant • Venus Express Project
References • Belyaev, D. et al., 2010, Vertical profiling of SO2 and SO above Venus' clouds by SPICAV/SOIR solar occultations, Icarus, In press. • Krasnopolsky, V.A., 2011, Vertical profile of H2SO4 vapor at 70–110 km on Venus and some related problems. Icarus, doi:10.1016/j.icarus.2011.06.036 • Sandor, B. J., et al., 2010, Sulfur chemistry in the Venus mesosphere from SO2 and SO microwave spectra, Icarus 208, 49-60. • Sandor, B.J., Clancy, R.T., Moriarty-Schieven, G.H., 2011, Upper limits for H2SO4 in the mesosphere of Venus. Icarus. doi:10.1016/j.icarus.2011.03.032. • Zhang, X., et al., 2011, Sulfur chemistry in the middle atmosphere of Venus. Icarus, doi:10.1016/j.icarus.2011.06.016.