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| 題名: | Top-down constraints on atmospheric mercury emissions and implications for global biogeochemical cycling |
| 作者: | 許桂榮;Song, Shaoije;Kelley, Paul;Wip, Dennis;Selin, Noelle E.;Luke, Winston T.;Holsen, Thomas M.;Kang, Shichang;Soerensen, Anne L.;Slemr, Franz;Pfaffhuber, Katrine Aspmo;Marumoto, Kohji;Angot, Hélène;Warneke, Thorsten;Jaffe, Daniel A.;Zhang, Qianggong;Conley, Gary D.;Dommergue, Aurélien;Weigelt, Andreas;Magand, Olivier;Brunke, Ernst Günther;Ebinghaus, Ralf;Ren, Xinrong;Artz, Richard S.;Peter, Weiss-Penzias;Sheu, Guey Rong;Brooks, Steven |
| 貢獻者: | 地球科學學院大氣科學學系 |
| 關鍵詞: | [SDE] Environmental Sciences;Chemistry;Physics;QC1-999;QD1-999;Trollobservatoriet;Zeppelinobservatoriet |
| 日期: | 2015-06-30 |
| 上傳時間: | 2026-04-21 14:06:00 (UTC+8) |
| 出版者: | European Geosciences Union;Copernicus GmbH |
| 摘要: | 摘要： Abstract. We perform global-scale inverse modeling to constrain present-day atmospheric mercury emissions and relevant physio-chemical 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.
出版者： Copernicus GmbH
出版日期： 2015-02-25
出處： Atmospheric Chemistry and Physics, 2015-02, Vol.15, p.7103-7125
資源來源： Agricultural & environmental science database online journals
識別號： EISSN: 1680-7324
識別號： DOI: 10.5194/acpd-15-5269-2015
識別號： DOI: 10.5194/acp-15-7103-2015 |
| 顯示於類別: | [大氣科學學系] 期刊論文
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