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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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amtd-2-2539-2009</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/2/2539/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/2/2539/2009/amtd-2-2539-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/2/2539/2009/amtd-2-2539-2009.pdf</fulltext_pdf>
	<start_page>2539</start_page>
	<end_page>2586</end_page>
	<publication_date>2009-10-08</publication_date>
	<article_title content_type="html">Intercomparison of measurements of NO&lt;sub&gt;2&lt;/sub&gt; concentrations in the atmosphere simulation chamber SAPHIR during the NO3Comp campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,11">
			<name>H. Fuchs</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>S. M. Ball</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>B. Bohn</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>T. Brauers</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>R. C. Cohen</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>H.-P. Dorn</name>
		</author>
		<author numeration="7" affiliations="1,2">
			<name>W. P. DubÃ©</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>J. L. Fry</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>R. HÃ¤seler</name>
		</author>
		<author numeration="10" affiliations="6">
			<name>U. Heitmann</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>R. L. Jones</name>
		</author>
		<author numeration="12" affiliations="8">
			<name>J. Kleffmann</name>
		</author>
		<author numeration="13" affiliations="4">
			<name>T. F. Mentel</name>
		</author>
		<author numeration="14" affiliations="4">
			<name>P. MÃ¼sgen</name>
		</author>
		<author numeration="15" affiliations="4">
			<name>F. Rohrer</name>
		</author>
		<author numeration="16" affiliations="5">
			<name>A. W. Rollins</name>
		</author>
		<author numeration="17" affiliations="6,9">
			<name>A. A. Ruth</name>
		</author>
		<author numeration="18" affiliations="4">
			<name>A. Kiendler-Scharr</name>
		</author>
		<author numeration="19" affiliations="4">
			<name>E. Schlosser</name>
		</author>
		<author numeration="20" affiliations="7">
			<name>A. J. L. Shillings</name>
		</author>
		<author numeration="21" affiliations="4">
			<name>R. Tillmann</name>
		</author>
		<author numeration="22" affiliations="6,9">
			<name>R. M. Varma</name>
		</author>
		<author numeration="23" affiliations="9,10">
			<name>D. S. Venables</name>
		</author>
		<author numeration="24" affiliations="8">
			<name>G. Villena Tapia</name>
		</author>
		<author numeration="25" affiliations="4">
			<name>A. Wahner</name>
		</author>
		<author numeration="26" affiliations="4">
			<name>R. Wegener</name>
		</author>
		<author numeration="27" affiliations="5">
			<name>P. J. Wooldridge</name>
		</author>
		<author numeration="28" affiliations="1">
			<name>S. S. Brown</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Oceanic and Atmospheric Administration, Earth System Research Laboratory, Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Institute for Research in the Environmental Sciences, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry, University of Leicester, Leicester, UK</affiliation>
		<affiliation numeration="4" content_type="html">Institut fÃ¼r Chemie und Dynamik der GeosphÃ¤re 2, Forschungszentrum JÃ¼lich GmbH, JÃ¼lich, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Department of Chemistry, University of California Berkeley, Berkeley, CA, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Physics, University College Cork, Cork, Ireland</affiliation>
		<affiliation numeration="7" content_type="html">Department of Chemistry, University of Cambridge, Cambridge, UK</affiliation>
		<affiliation numeration="8" content_type="html">Physikalische Chemie/Fachbereich C, Bergische UniversitÃ¤t Wuppertal, Wuppertal, Germany</affiliation>
		<affiliation numeration="9" content_type="html">Department of Chemistry, University College Cork, Cork, Ireland</affiliation>
		<affiliation numeration="10" content_type="html">Environmental Research Institute, University College Cork, Cork, Ireland</affiliation>
		<affiliation numeration="11" content_type="html">now at: Institut fÃ¼r Chemie und Dynamik der GeosphÃ¤re 2, Forschungszentrum JÃ¼lich GmbH, JÃ¼lich, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">NO&lt;sub&gt;2&lt;/sub&gt; concentrations were measured by various instruments during the NO3Comp campaign
at the atmosphere simulation chamber SAPHIR at Forschungszentrum JÃ¼lich, Germany, in June
2007. Analytic methods included photolytic conversion with chemiluminescence (PC-CLD),
broadband cavity ring-down spectroscopy (BBCRDS), pulsed cavity ring-down spectroscopy
(CRDS), incoherent broadband cavity-enhanced absorption spectroscopy (IBBCEAS), and
laser-induced fluorescence (LIF). All broadband absorption spectrometers were optimized for
the detection of the main target species of the campaign, NO&lt;sub&gt;2&lt;/sub&gt;, but were also capable
of detecting NO&lt;sub&gt;2&lt;/sub&gt; simultaneously with reduced sensitivity. NO&lt;sub&gt;2&lt;/sub&gt; mixing ratios
in the chamber were within a range characteristic of polluted, urban conditions, with
a maximum mixing ratio of approximately 75 ppbv. The overall agreement between
measurements of all instruments was excellent. Linear fits of the combined data sets
resulted in slopes that differ from unity only within the stated uncertainty of each
instrument. Possible interferences from species such as water vapor and ozone were
negligible under the experimental conditions.</abstract>
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