<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-1241-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/1241/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/1241/2005/acpd-5-1241-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/1241/2005/acpd-5-1241-2005.pdf</fulltext_pdf>
	<start_page>1241</start_page>
	<end_page>1253</end_page>
	<publication_date>2005-03-09</publication_date>
	<article_title content_type="html">Evidence for long-lived polar vortex air in the mid-latitude summer stratosphere from in situ laser diode CH&lt;sub&gt;4&lt;/sub&gt; and H&lt;sub&gt;2&lt;/sub&gt;O measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>G. Durry</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Hauchecorne</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">IPSL, Service d’A&amp;eacute;ronomie, UMR 7620, BP 3, 91371 Verri&amp;egrave;res-le-Buisson C&amp;eacute;dex, France</affiliation>
		<affiliation numeration="2" content_type="html">GSMA, UMR 6089, Universit&amp;eacute; de Reims, BP 1039, 51687 Reims, C&amp;eacute;dex 2, France</affiliation>
	</affiliations>
	<abstract content_type="html">A balloon borne diode laser spectrometer was launched in southern France in
June 2000 to yield in situ stratospheric CH&lt;sub&gt;4&lt;/sub&gt; and H&lt;sub&gt;2&lt;/sub&gt;O measurements.
In the altitude region ranging from 20 km to 25 km, striking large spatial
structures were observed in the vertical concentration profiles of both
species. We suggest these patterns are due to the presence of long-lived
remnants of the wintertime polar vortex in the mid-latitude summer
stratosphere. To support this interpretation, a high resolution advection
model for potential vorticity is used to investigate the evolution of the
Arctic vortex after its breakdown phase in spring 2000.</abstract>
	<references>
	</references>
</article>

