Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 42, Issue 23, Pages 10494-10502Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL066645
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Funding
- U.S. National Science Foundation [1217010, 1215712]
- Directorate For Geosciences
- Div Atmospheric & Geospace Sciences [1215712] Funding Source: National Science Foundation
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [1217010, 1216707, 1216166] Funding Source: National Science Foundation
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Mercury is a global toxin that can be introduced to ecosystems through atmospheric deposition. Mercury oxidation is thought to occur in the free troposphere by bromine radicals, but direct observational evidence for this process is currently unavailable. During the 2013 Nitrogen, Oxidants, Mercury and Aerosol Distributions, Sources and Sinks campaign, we measured enhanced oxidized mercury and bromine monoxide in a free tropospheric air mass over Texas. We use trace gas measurements, air mass back trajectories, and a chemical box model to confirm the origin and chemical history of the sampled air mass. We find the presence of elevated oxidized mercury to be consistent with oxidation of elemental mercury by bromine atoms in this subsiding upper tropospheric air mass within the subtropical Pacific High, where dry atmospheric conditions are conducive to oxidized mercury accumulation. Our results support the role of bromine as the dominant oxidant of mercury in the upper troposphere.
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