Atmos. Chem. Phys., 13, 5551-5565, 2013
www.atmos-chem-phys.net/13/5551/2013/
doi:10.5194/acp-13-5551-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Southern hemispheric halon trends and global halon emissions, 1978–2011
M. J. Newland1, C. E. Reeves1, D. E. Oram2, J. C. Laube1, W. T. Sturges1, C. Hogan1, P. Begley1, and P. J. Fraser3
1School of Environmental Sciences, University of East Anglia, Norwich, UK
2National Centre for Atmospheric Science, School of Environmental Sciences, University of East Anglia, Norwich, UK
3Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, Victoria, Australia

Abstract. The atmospheric records of four halons, H-1211 (CBrClF2), H-1301 (CBrF3), H-2402 (CBrF2CBrF2) and H-1202 (CBr2F2), measured from air collected at Cape Grim, Tasmania, between 1978 and 2011, are reported. Mixing ratios of H-1211, H-2402 and H-1202 began to decline in the early to mid-2000s, but those of H-1301 continue to increase up to mid-2011. These trends are compared to those reported by NOAA (National Oceanic and Atmospheric Administration) and AGAGE (Advanced Global Atmospheric Experiment). The observations suggest that the contribution of the halons to total tropospheric bromine at Cape Grim has begun to decline from a peak in 2008 of about 8.1 ppt. An extrapolation of halon mixing ratios to 2060, based on reported banks and predicted release factors, shows this decline becoming more rapid in the coming decades, with a contribution to total tropospheric bromine of about 3 ppt in 2060. Top-down global annual emissions of the halons were derived using a two-dimensional atmospheric model. The emissions of all four have decreased since peaking in the late 1980s–mid-1990s, but this decline has slowed recently, particularly for H-1301 and H-2402 which have shown no decrease in emissions over the past five years. The UEA (University of East Anglia) top-down model-derived emissions are compared to those reported using a top-down approach by NOAA and AGAGE and the bottom-up estimates of HTOC (Halons Technical Options Committee). The implications of an alternative set of steady-state atmospheric lifetimes are discussed. Using a lifetime of 14 yr or less for H-1211 to calculate top-down emissions estimates would lead to small, or even negative, estimated banks given reported production data. Finally emissions of H-1202, a product of over-bromination during the production process of H-1211, have continued despite reported production of H-1211 ceasing in 2010. This raises questions as to the source of these H-1202 emissions.

Citation: Newland, M. J., Reeves, C. E., Oram, D. E., Laube, J. C., Sturges, W. T., Hogan, C., Begley, P., and Fraser, P. J.: Southern hemispheric halon trends and global halon emissions, 1978–2011, Atmos. Chem. Phys., 13, 5551-5565, doi:10.5194/acp-13-5551-2013, 2013.
 
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