How marine emissions of bromoform impact the remote atmosphere
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Published:2019-09-03
Issue:17
Volume:19
Page:11089-11103
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Jia YueORCID, Tegtmeier Susann, Atlas ElliotORCID, Quack Birgit
Abstract
Abstract. It is an open question how localized elevated emissions of bromoform (CHBr3) and other very short-lived halocarbons (VSLHs), found in coastal and upwelling regions, and low background
emissions, typically found over the open ocean, impact the atmospheric
VSLH distribution. In this study, we use the Lagrangian dispersion model
FLEXPART to simulate atmospheric CHBr3 resulting from assumed uniform background emissions, and from elevated emissions consistent with those derived during three tropical cruise campaigns. The simulations demonstrate that the atmospheric CHBr3 distributions in the uniform background emissions scenario are highly variable with high mixing ratios appearing in regions of convergence or low wind speed. This relation holds on regional and global scales. The impact of localized elevated emissions on the atmospheric CHBr3
distribution varies significantly from campaign to campaign. The estimated
impact depends on the strength of the emissions and the meteorological
conditions. In the open waters of the western Pacific and Indian oceans,
localized elevated emissions only slightly increase the background
concentrations of atmospheric CHBr3, even when 1∘ wide source
regions along the cruise tracks are assumed. Near the coast, elevated
emissions, including hot spots up to 100 times larger than the uniform
background emissions, can be strong enough to be distinguished from the
atmospheric background. However, it is not necessarily the highest hot spot
emission that produces the largest enhancement, since the tug-of-war between fast advective transport and local accumulation at the time of emission is also important. Our results demonstrate that transport variations in the atmosphere itself
are sufficient to produce highly variable VSLH distributions, and elevated
VSLHs in the atmosphere do not always reflect a strong localized source.
Localized elevated emissions can be obliterated by the highly variable
atmospheric background, even if they are orders of magnitude larger than the average open ocean emissions.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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