Atmos. Chem. Phys. Discuss., 12, 11595-11639, 2012
www.atmos-chem-phys-discuss.net/12/11595/2012/
doi:10.5194/acpd-12-11595-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Iodine emissions from the sea ice of the Weddell Sea
H. M. Atkinson1,2, R.-J. Huang3, R. Chance4,*, H. K. Roscoe1, C. Hughes2,**, B. Davison5, A. Schönhardt6, A. S. Mahajan7, A. Saiz-Lopez7, T. Hoffmann3, and P. S. Liss2
1British Antarctic Survey, Cambridge, UK
2University of East Anglia, Norwich, UK
3Johannes Gutenberg University of Mainz, Germany
4University of York, UK
5Lancaster University, UK
6University of Bremen, Germany
7Laboratory for Atmospheric and Climate Science, CSIC, Toledo, Spain
*now at: University of East Anglia, Norwich, UK
**now at: University of York, UK

Abstract. Iodine compounds were measured above, below and within the sea ice of the Weddell Sea during a cruise in 2009, to elucidate the mechanism of local enhancement and volatilisation of iodine. I2 mixing ratios of up to 12.4 pptv were measured 10 m above the sea ice, and up to 31 pptv was observed above surface snow on the nearby Brunt Ice Shelf – large amounts. Atmospheric IO of up to 7 pptv was measured from the ship, and the average sum of HOI and ICl was 1.9 pptv. These measurements confirm the Weddell Sea as an iodine hotspot. Average atmospheric concentrations of CH3I, C2H5I, CH2ICl, 2-C3H7I, CH2IBr and 1-C3H7I were each 0.2 pptv or less. On the Brunt Ice Shelf, enhanced concentrations of CH3I and C2H5I (up to 0.5 and 1 pptv, respectively) were observed in firn air, with a diurnal profile that suggests the snow may be a source. In the sea ice brine, iodocarbons concentrations were over 10 times those of the sea water below. The sum of iodide + iodate was depleted in sea ice samples, suggesting some missing iodine chemistry. Flux calculations suggest I2 dominates the iodine atom flux to the atmosphere, but models cannot reconcile the observations and suggest either a missing iodine source or other deficiencies in our understanding of iodine chemistry. The observation of new particle formation, consistent with the model predictions, strongly suggests an iodine source. This combined study of iodine compounds is the first of its kind in this unique region of sea ice rich in biology and rich in iodine chemistry.

Citation: Atkinson, H. M., Huang, R.-J., Chance, R., Roscoe, H. K., Hughes, C., Davison, B., Schönhardt, A., Mahajan, A. S., Saiz-Lopez, A., Hoffmann, T., and Liss, P. S.: Iodine emissions from the sea ice of the Weddell Sea, Atmos. Chem. Phys. Discuss., 12, 11595-11639, doi:10.5194/acpd-12-11595-2012, 2012.
 
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