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    • A new interpretation of total column BrO during Arctic spring 

      Salawitch, R. J.; Canty, T.; Kurosu, T; Chance, Kelly V.; Liang, Q.; da Silva, A.; Pawson, S.; Nielsen, J. E.; Rodriguez, J. M.; Bhartia, P. K.; Liu, X.; Huey, L. G.; Liao, J.; Stickel, R. E.; Tanner, D. J.; Dibb, J. E.; Simpson, W. R.; Donohoue, D.; Weinheimer, A.; Flocke, F.; Knapp, D.; Montzka, D.; Neuman, J. A.; Nowak, J. B.; Ryerson, T. B.; Oltmans, S.; Blake, D. R.; Atlas, E. L.; Kinnison, D. E.; Tilmes, S.; Pan, L. L.; Hendrick, F.; Van Roozendael, M.; Kreher, K.; Johnston, P. V.; Gao, R. S.; Johnson, B.; Bui, T. P.; Chen, G.; Pierce, R. B.; Crawford, J. H.; Jacob, Daniel James (Wiley-Blackwell, 2010)
      Emission of bromine from sea-salt aerosol, frost flowers, ice leads, and snow results in the nearly complete removal of surface ozone during Arctic spring. Regions of enhanced total column BrO observed by satellites have ...