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Top-down constraints on atmospheric mercury emissions and implications for global biogeochemical cycling

S Song. 1 Ne Selin 2, 1 A.L Soerensen 3, 4 Hélène Angot 5 R Artz 6 S. Brooks 7 E.-G. Brunke 8 G Conley 9 Aurelien Dommergue 5 R. Ebinghaus 10 T.M Holsen 11 D. Jaffe 12 S. Kang 13 P. Kelley 14 Wt Luke 14 Olivier Magand 5 K. Marumoto 15 Ka Pfaffhuber 16 X Ren 17, 14 Gr Sheu 18 F. Slemr 19 T. Warneke 20 A Weigelt 10 P Weiss-Penzias 21 Dc Wip 22 Q. P. Zhang 23 
Abstract : We perform global-scale inverse modeling to constrain present-day atmospheric mercury emissions and relevant physiochemical parameters in the GEOS-Chem chemical transport model. We use Bayesian inversion methods combining simulations with GEOS-Chem and ground-based Hg0 observations from regional monitoring networks and individual sites in recent years. Using optimized emissions/parameters, GEOS-Chem better reproduces these ground-based observations and also matches regional over-water Hg0 and wet deposition measurements. The optimized global mercury emission to the atmosphere is ~ 5.8 Gg yr−1. The ocean accounts for 3.2 Gg yr−1 (55 % of the total), and the terrestrial ecosystem is neither a net source nor a net sink of Hg0. The optimized Asian anthropogenic emission of Hg0 (gas elemental mercury) is 650–1770 Mg yr−1, higher than its bottom-up estimates (550–800 Mg yr−1). The ocean parameter inversions suggest that dark oxidation of aqueous elemental mercury is faster, and less mercury is removed from the mixed layer through particle sinking, when compared with current simulations. Parameter changes affect the simulated global ocean mercury budget, particularly mass exchange between the mixed layer and subsurface waters. Based on our inversion results, we re-evaluate the long-term global biogeochemical cycle of mercury, and show that legacy mercury becomes more likely to reside in the terrestrial ecosystem than in the ocean. We estimate that primary anthropogenic mercury contributes up to 23 % of present-day atmospheric deposition.
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S Song., Ne Selin, A.L Soerensen, Hélène Angot, R Artz, et al.. Top-down constraints on atmospheric mercury emissions and implications for global biogeochemical cycling. Atmospheric Chemistry and Physics, European Geosciences Union, 2015, 15 (12), pp.7103-7125. ⟨10.5194/acp-15-7103-2015⟩. ⟨insu-01203657⟩



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