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Particles and iodine compounds in coastal Antarctica

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journal contribution
posted on 2019-09-30, 11:36 authored by HK Roscoe, AE Jones, N Brough, R Weller, A Saiz-Lopez, AS Mahajan, A Schoenhardt, JP Burrows, ZL Fleming
Aerosol particle number concentrations have been measured at Halley and Neumayer on the Antarctic coast, since 2004 and 1984, respectively. Sulphur compounds known to be implicated in particle formation and growth were independently measured: sulphate ions and methane sulphonic acid in filtered aerosol samples and gas phase dimethyl sulphide for limited periods. Iodine oxide, IO, was determined by a satellite sensor from 2003 to 2009 and by different ground‐based sensors at Halley in 2004 and 2007. Previous model results and midlatitude observations show that iodine compounds consistent with the large values of IO observed may be responsible for an increase in number concentrations of small particles. Coastal Antarctica is useful for investigating correlations between particles, sulphur, and iodine compounds, because of their large annual cycles and the source of iodine compounds in sea ice. After smoothing all the measured data by several days, the shapes of the annual cycles in particle concentration at Halley and Neumayer are approximated by linear combinations of the shapes of sulphur compounds and IO but not by sulphur compounds alone. However, there is no short‐term correlation between IO and particle concentration. The apparent correlation by eye after smoothing but not in the short term suggests that iodine compounds and particles are sourced some distance offshore. This suggests that new particles formed from iodine compounds are viable, i.e., they can last long enough to grow to the larger particles that contribute to cloud condensation nuclei, rather than being simply collected by existing particles. If so, there is significant potential for climate feedback near the sea ice zone via the aerosol indirect effect.

History

Citation

Journal of Geophysical Research: Atmospheres, 2015, 120 (14), pp. 7144-7156

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Chemistry

Version

  • VoR (Version of Record)

Published in

Journal of Geophysical Research: Atmospheres

Publisher

American Geophysical Union (AGU), Wiley

issn

2169-897X

Acceptance date

2015-06-29

Copyright date

2015

Available date

2019-09-30

Publisher version

https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2015JD023301

Notes

All data used in this paper can be accessed by contacting the authors responsible: measurements at Halley‐h.roscoe@bas.ac.uk; measurements at Neumayer‐Rolf.Weller@awi.de; SCIAMACHY data‐schoenhardt@iup.physik.uni-bremen.de; model output‐a.saiz‐lopez@ciac.jccm‐csic.es; and trajectory output‐zf5@leicester.ac.uk. Some Halley measurements are already available at the British Polar Data Centre (http://www.antarctica.ac.uk/bas_research/data/access/search.php), more will be posted during 2015.

Language

en

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