Articles | Volume 17, issue 24
https://doi.org/10.5194/acp-17-14955-2017
https://doi.org/10.5194/acp-17-14955-2017
Research article
 | 
19 Dec 2017
Research article |  | 19 Dec 2017

Cyclone-induced surface ozone and HDO depletion in the Arctic

Xiaoyi Zhao, Dan Weaver, Kristof Bognar, Gloria Manney, Luis Millán, Xin Yang, Edwin Eloranta, Matthias Schneider, and Kimberly Strong

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Cited articles

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Adams, C., Strong, K., Zhao, X., Bourassa, A. E., Daffer, W. H., Degenstein, D., Drummond, J. R., Farahani, E. E., Fraser, A., Lloyd, N. D., Manney, G. L., McLinden, C. A., Rex, M., Roth, C., Strahan, S. E., Walker, K. A., and Wohltmann, I.: The spring 2011 final stratospheric warming above Eureka: anomalous dynamics and chemistry, Atmos. Chem. Phys., 13, 611–624, https://doi.org/10.5194/acp-13-611-2013, 2013.
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Short summary
Few scientific questions about surface ozone depletion have been addressed, using a variety of measurements and atmospheric models. The lifetime of reactive bromine is only a few hours in the absence of recycling. Evidence of this recycling over aerosol or blowing-snow/ice particles was found at Eureka. The blowing snow sublimation process is a key step in producing bromine-enriched sea-salt aerosol. Ground-based FTIR isotopologue measurements at Eureka provided evidence of this key step.
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