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Organic iodine in Antarctic sea ice: A comparison between winter in the Weddell Sea and summer in the Amundsen Sea
Responsible organisation
2014 (English)In: Journal of Geophysical Research - Biogeosciences, ISSN 2169-8953, E-ISSN 2169-8961, Vol. 119, no 12, p. 2276-2291Article in journal (Refereed) Published
Abstract [en]

Recent studies have recognized sea ice as a source of reactive iodine to the Antarctic boundary layer. Volatile iodinated compounds (iodocarbons) are released from sea ice, and they have been suggested to contribute to the formation of iodine oxide (IO), which takes part in tropospheric ozone destruction in the polar spring. We measured iodocarbons (CH3I, CH2ClI, CH2BrI, and CH2I2) in sea ice, snow, brine, and air during two expeditions to Antarctica, OSO 10/11 to the Amundsen Sea during austral summer and ANT XXIX/6 to the Weddell Sea in austral winter. These are the first reported measurements of iodocarbons from the Antarctic winter. Iodocarbons were enriched in sea ice in relation to seawater in both summer and winter. During summer, the positive relationship to chlorophyll a biomass indicated a biological origin. We suggest that CH3I is formed biotically in sea ice during both summer and winter. For CH2ClI, CH2BrI, and CH2I2, an additional abiotic source at the snow/ice interface in winter is suggested. Elevated air concentrations of CH3I and CH2ClI during winter indicate that they are enriched in lower troposphere and may take part in the formation of IO at polar sunrise.

Place, publisher, year, edition, pages
2014. Vol. 119, no 12, p. 2276-2291
Keywords [en]
sea ice; organoiodine; halocarbons; chlorophyll a
National Category
Natural Sciences
Research subject
SWEDARP 2010/11, Oden Southern Ocean 2010/11
Identifiers
URN: urn:nbn:se:polar:diva-2936DOI: 10.1002/2014JG002727OAI: oai:DiVA.org:polar-2936DiVA, id: diva2:1046062
Available from: 2016-11-11 Created: 2016-10-27 Last updated: 2017-11-29

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