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<article language="en">
	<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>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-12707-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/12707/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/12707/2009/acpd-9-12707-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/12707/2009/acpd-9-12707-2009.pdf</fulltext_pdf>
	<start_page>12707</start_page>
	<end_page>12730</end_page>
	<publication_date>2009-06-04</publication_date>
	<article_title content_type="html">Simultaneous measurements of OClO, NO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; in the Arctic polar vortex by the GOMOS instrument</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Tétard</name>
			<email>cedric.tetard@aeronomie.be</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. Fussen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. Bingen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>N. Capouillez</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>E. Dekemper</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>N. Loodts</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>N. Mateshvili</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>F. Vanhellemont</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>E. Kyrölä</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>J. Tamminen</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>V. Sofieva</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>A. Hauchecorne</name>
		</author>
		<author numeration="13" affiliations="3">
			<name>F. Dalaudier</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>J.-L. Bertaux</name>
		</author>
		<author numeration="15" affiliations="4">
			<name>O. Fanton d&apos;Andon</name>
		</author>
		<author numeration="16" affiliations="4">
			<name>G. Barrot</name>
		</author>
		<author numeration="17" affiliations="4">
			<name>M. Guirlet</name>
		</author>
		<author numeration="18" affiliations="5">
			<name>T. Fehr</name>
		</author>
		<author numeration="19" affiliations="5">
			<name>L. Saavedra</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut d&apos;Aéronomie Spatiale de Belgique, Brussels, Belgium</affiliation>
		<affiliation numeration="2" content_type="html">Finnish Meteorological Institute, Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">Service d&apos;Aéronomie du CNRS, Verrières-le-buisson, France</affiliation>
		<affiliation numeration="4" content_type="html">ACRI-ST, Sophia-Antipolis, France</affiliation>
		<affiliation numeration="5" content_type="html">European Space Research Institute (ESRIN), European Space Agency, Frascaty, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">We present the first nighttime measurements of OClO from a limb-viewing
satellite instrument in the Arctic polar vortex. The relationship between
OClO, NO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; slant column densities in the Arctic polar vortex are
analyzed from the GOMOS measurements. The retrieval process is based on a
differential optical absorption spectroscopy (DOAS) method applied on the
weighted median GOMOS transmittances. A study about the longitudinal
distributions of OClO, NO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; above 65&amp;deg; north in January
2008 is presented. It shows a strong halogen activation in the lower
stratosphere and a strong denoxification in the entire stratosphere inside
the Arctic polar vortex. Time series of temperatures and OClO, NO&lt;sub&gt;2&lt;/sub&gt; and
O&lt;sub&gt;3&lt;/sub&gt; slant column densities for the winters 2002/2003 to 2007/2008 are also
presented. They highlight the correlation between temperature, OClO and
NO&lt;sub&gt;2&lt;/sub&gt;. The GOMOS instrument appears to be a very suitable instrument for the
monitoring of OClO, NO&lt;sub&gt;2&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; in the stratosphere during nighttime.</abstract>
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</article>

