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	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-17125-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/17125/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/17125/2009/acpd-9-17125-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/17125/2009/acpd-9-17125-2009.pdf</fulltext_pdf>
	<start_page>17125</start_page>
	<end_page>17155</end_page>
	<publication_date>2009-08-14</publication_date>
	<article_title content_type="html">Coastal measurements of short-lived reactive iodocarbons and bromocarbons at Roscoff, Brittany during the RHaMBLe campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. E. Jones</name>
			<email>cej103@york.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>K. E. Hornsby</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>R. M. Dunk</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>R. J. Leigh</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>L. J. Carpenter</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, University of York, Heslington, York, YO10 5DD, UK</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics and Astronomy, University of Leicester, Leicester, LE1 7RH, UK</affiliation>
		<affiliation numeration="3" content_type="html">now at: Crichton Carbon Centre, Crichton University Campus, Dumfries, DG1 4ZL, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Atmospheric concentrations of the volatile reactive iodocarbons
C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;5&lt;/sub&gt;I, 1-C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;7&lt;/sub&gt;I, 2-C&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;7&lt;/sub&gt;I, CH&lt;sub&gt;2&lt;/sub&gt;ICl,
CH&lt;sub&gt;2&lt;/sub&gt;IBr, CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt; and bromocarbons CH&lt;sub&gt;2&lt;/sub&gt;Br&lt;sub&gt;2&lt;/sub&gt; and
CHBr&lt;sub&gt;3&lt;/sub&gt; were determined by GC/MS analysis of marine boundary layer air at
Roscoff, Brittany on the northwest coast of France during September 2006.
Comparison with other coastal studies suggests that emissions of these trace
gases are strongly influenced by site topography, seaweed populations and
distribution, as well as tide height. Concentrations of the very short-lived
dihalomethanes CH&lt;sub&gt;2&lt;/sub&gt;IBr and CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt; in particular showed evidence
of tidal dependence, with higher concentrations observed at low tide during
maximum exposure of seaweed beds. We also present a limited number of
halocarbon concentrations in surface seawater and estimate sea-air fluxes
based on simultaneous water and air measurements of these gases.
CH&lt;sub&gt;2&lt;/sub&gt;Br&lt;sub&gt;2&lt;/sub&gt; and CHBr&lt;sub&gt;3&lt;/sub&gt; were strongly correlated both in air and in
seawater, with CH&lt;sub&gt;2&lt;/sub&gt;Br&lt;sub&gt;2&lt;/sub&gt;/CHBr&lt;sub&gt;3&lt;/sub&gt; ratios of 0.19 in air and 0.06 in
water. The combined midday I atom flux from the photolabile diahlomethanes
CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;2&lt;/sub&gt;IBr and CH&lt;sub&gt;2&lt;/sub&gt;ICl of ~5&amp;times;10&lt;sup&gt;3&lt;/sup&gt; molecules cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
is several orders of magnitude lower than the
estimated I atom flux from I&lt;sub&gt;2&lt;/sub&gt; based on coinciding measurements at the
same site, which indicates that at Roscoff the major I atom precursor was
I&lt;sub&gt;2&lt;/sub&gt; rather than reactive iodocarbons.</abstract>
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