Modeling the global atmospheric transport and deposition of mercury to the Great Lakes

Author:

Cohen Mark D.1,Draxler Roland R.1,Artz Richard S.1,Blanchard Pierrette2,Gustin Mae Sexauer3,Han Young-Ji45,Holsen Thomas M.4,Jaffe Daniel A.6,Kelley Paul17,Lei Hang1,Loughner Christopher P.18,Luke Winston T.1,Lyman Seth N.9,Niemi David10,Pacyna Jozef M.1112,Pilote Martin10,Poissant Laurier10,Ratte Dominique10,Ren Xinrong17,Steenhuisen Frits13,Steffen Alexandra2,Tordon Rob14,Wilson Simon J.15

Affiliation:

1. National Oceanic and Atmospheric Administration (NOAA), Maryland, United States of America

2. Environment and Climate Change Canada, Ontario, Canada

3. University of Nevada-Reno, Nevada, United States of America

4. Clarkson University, New York, United States of America

5. Kangwon National University, South Korea

6. University of Washington, Washington, United States of America

7. Cooperative Institute for Climate and Satellites, University of Maryland, Maryland, United States of America

8. Earth System Science Interdisciplinary Center (ESSIC), University of Maryland, Maryland, United States of America

9. Utah State University, Utah, United States of America

10. Environment and Climate Change Canada, Quebec, Canada

11. Norwegian Institute for Air Research (NILU), Norway

12. Gdansk University of Technology, Poland

13. Arctic Centre, University of Groningen, Netherlands

14. Environment and Climate Change Canada, Nova Scotia, Canada

15. Arctic Monitoring and Assessment Program (AMAP), Norway

Abstract

Abstract Mercury contamination in the Great Lakes continues to have important public health and wildlife ecotoxicology impacts, and atmospheric deposition is a significant ongoing loading pathway. The objective of this study was to estimate the amount and source-attribution for atmospheric mercury deposition to each lake, information needed to prioritize amelioration efforts. A new global, Eulerian version of the HYSPLIT-Hg model was used to simulate the 2005 global atmospheric transport and deposition of mercury to the Great Lakes. In addition to the base case, 10 alternative model configurations were used to examine sensitivity to uncertainties in atmospheric mercury chemistry and surface exchange. A novel atmospheric lifetime analysis was used to characterize fate and transport processes within the model. Model-estimated wet deposition and atmospheric concentrations of gaseous elemental mercury (Hg(0)) were generally within ∼10% of measurements in the Great Lakes region. The model overestimated non-Hg(0) concentrations by a factor of 2–3, similar to other modeling studies. Potential reasons for this disagreement include model inaccuracies, differences in atmospheric Hg fractions being compared, and the measurements being biased low. Lake Erie, downwind of significant local/regional emissions sources, was estimated by the model to be the most impacted by direct anthropogenic emissions (58% of the base case total deposition), while Lake Superior, with the fewest upwind local/regional sources, was the least impacted (27%). The U.S. was the largest national contributor, followed by China, contributing 25% and 6%, respectively, on average, for the Great Lakes. The contribution of U.S. direct anthropogenic emissions to total mercury deposition varied between 46% for the base case (with a range of 24–51% over all model configurations) for Lake Erie and 11% (range 6–13%) for Lake Superior. These results illustrate the importance of atmospheric chemistry, as well as emissions strength, speciation, and proximity, to the amount and source-attribution of mercury deposition.

Publisher

University of California Press

Subject

Atmospheric Science,Geology,Geotechnical Engineering and Engineering Geology,Ecology,Environmental Engineering,Oceanography

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