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	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>7</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acp-7-443-2007</doi>
	<article_url>http://www.atmos-chem-phys.net/7/443/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/7/443/2007/acp-7-443-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/7/443/2007/acp-7-443-2007.pdf</fulltext_pdf>
	<start_page>443</start_page>
	<end_page>451</end_page>
	<publication_date>2007-01-25</publication_date>
	<article_title content_type="html">Water-side turbulence enhancement of ozone deposition to the ocean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. W. Fairall</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. Helmig</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>L. Ganzeveld</name>
		</author>
		<author numeration="4" affiliations="4,5">
			<name>J. Hare</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NOAA Earth Science Research Laboratory, Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">INSTAAR, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Max-Planck Institute for Chemistry, Mainz, Germany</affiliation>
		<affiliation numeration="4" content_type="html">CIRES, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="5" content_type="html">now at: SOLAS International Project Office, University of East Anglia, Norwich, UK</affiliation>
	</affiliations>
	<abstract content_type="html">A parameterization for the deposition velocity of an ocean-reactive
atmospheric gas (such as ozone) is developed. The parameterization is based
on integration of the turbulent-molecular transport equation (with a
chemical source term) in the ocean. It extends previous work that only
considered reactions within the oceanic molecular sublayer. The sensitivity
of the ocean-side transport to reaction rate and wind forcing is examined. A
more complicated case with a much more reactive thin surfactant layer is
also considered. The full atmosphere-ocean deposition velocity is obtained
by matching boundary conditions at the interface. For an assumed ocean
reaction rate of 10&lt;sup&gt;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, the enhancement for ozone deposition by
oceanic turbulence is found to be up to a factor of three for meteorological
data obtained in a recent cruise off the East Coast of the U.S.</abstract>
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</article>

