Interactions of bromine, chlorine, and iodine photochemistry during ozone depletions in Barrow, Alaska

Interactions of bromine, chlorine, and iodine photochemistry during ozone depletions in Barrow, Alaska

The springtime depletion of tropospheric ozone in the Arctic is known to be caused by active halogen photochemistry resulting from halogen atom precursors emitted from snow, ice, or aerosol surfaces. The role of bromine in driving ozone depletion events (ODEs) has been generally accepted, but much l...

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Bibliographic Details
Main Authors: C. R. Thompson, P. B. Shepson, J. Liao, L. G. Huey, E. C. Apel, C. A. Cantrell, F. Flocke, J. Orlando, A. Fried, S. R. Hall, R. S. Hornbrook, D. J. Knapp, R. L. Mauldin III, D. D. Montzka, B. C. Sive, K. Ullmann, P. Weibring, A. Weinheimer
Format: Article
Language:English
Published: Copernicus Publications 2015-08-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/9651/2015/acp-15-9651-2015.pdf

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http://www.atmos-chem-phys.net/15/9651/2015/acp-15-9651-2015.pdf

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