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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 4
Atmos. Chem. Phys., 15, 2215-2224, 2015
https://doi.org/10.5194/acp-15-2215-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 15, 2215-2224, 2015
https://doi.org/10.5194/acp-15-2215-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Feb 2015

Research article | 27 Feb 2015

A negative feedback between anthropogenic ozone pollution and enhanced ocean emissions of iodine

C. Prados-Roman1, C. A. Cuevas1, R. P. Fernandez1,*, D. E. Kinnison2, J-F. Lamarque2, and A. Saiz-Lopez1 C. Prados-Roman et al.
  • 1Atmospheric Chemistry and Climate Group, Institute of Physical Chemistry Rocasolano (CSIC), Madrid, Spain
  • 2Atmospheric Division, NCAR, Boulder, CO, USA
  • *now at: National Scientific and Technical Research Council (CONICET), UTN-FR Mendoza/ICB-UNCuyo, Mendoza, Argentina

Abstract. Naturally emitted from the oceans, iodine compounds efficiently destroy atmospheric ozone and reduce its positive radiative forcing effects in the troposphere. Emissions of inorganic iodine have been experimentally shown to depend on the deposition to the oceans of tropospheric ozone, whose concentrations have significantly increased since 1850 as a result of human activities. A chemistry–climate model is used herein to quantify the current ocean emissions of inorganic iodine and assess the impact that the anthropogenic increase in tropospheric ozone has had on the natural cycle of iodine in the marine environment since pre-industrial times. Our results indicate that the human-driven enhancement of tropospheric ozone has doubled the oceanic inorganic iodine emissions following the reaction of ozone with iodide at the sea surface. The consequent build-up of atmospheric iodine, with maximum enhancements of up to 70% with respect to pre-industrial times in continental pollution outflow regions, has in turn accelerated the ozone chemical loss over the oceans with strong spatial patterns. We suggest that this ocean–atmosphere interaction represents a negative geochemical feedback loop by which current ocean emissions of iodine act as a natural buffer for ozone pollution and its radiative forcing in the global marine environment.

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