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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>2</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amtd-2-1933-2009</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/2/1933/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/2/1933/2009/amtd-2-1933-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/2/1933/2009/amtd-2-1933-2009.pdf</fulltext_pdf>
	<start_page>1933</start_page>
	<end_page>1972</end_page>
	<publication_date>2009-08-19</publication_date>
	<article_title content_type="html">Determination of oceanic ozone deposition by ship-borne eddy covariance flux measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Bariteau</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. Helmig</name>
			<email>detlev.helmig@colorado.edu</email>
		</author>
		<author numeration="3" affiliations="3">
			<name>C. W. Fairall</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. E. Hare</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>J. Hueber</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>E. K. Lang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Alpine and Arctic Research (INSTAAR), University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">National Oceanic and Atmospheric Administration (NOAA), Earth System Research Laboratory (ESRL), Boulder, Colorado, USA</affiliation>
	</affiliations>
	<abstract content_type="html">A fast response ozone analyzer based on the ozone-nitric oxide chemiluminescence
method was integrated into the NOAA-ESRL flux system to achieve the first ship-borne,
direct ozone flux measurements over the open ocean. Air was collected from an inlet
at 18 m height over the ocean surface mounted to the bow-jackstaff and via a
30 m-long sampling line to the ozone instrument on the ship deck.
A &quot;puff&quot; system was used for accurate and regular determination of the sample
transport time (lag) between the inlet and the chemical analyzer. A Nafion-membrane
dryer facilitated removal of fast water vapor fluctuations, which eliminated the
need for quenching and density correction of the ozone signal. The sampling-analyzer
system was found to have a ~0.25–0.40 s response time at a sensitivity of
~2800 counts s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; per ppbv of ozone. Quality control and data filtering
procedures for eliminating data that did not meet measurement requirements were
critically evaluated. The new ozone flux system was deployed during several cruises
aboard the NOAA Ship &lt;i&gt;Ronald H. Brown&lt;/i&gt;, and evaluated using results obtained during
several research cruises off the coasts of the North and South America continents.</abstract>
	<references>
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</article>

