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<article language="en">
	<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>5</volume_number>
		<issue_number>10</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-2797-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/2797/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/2797/2005/acp-5-2797-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/2797/2005/acp-5-2797-2005.pdf</fulltext_pdf>
	<start_page>2797</start_page>
	<end_page>2807</end_page>
	<publication_date>2005-10-25</publication_date>
	<article_title content_type="html">Technical note: A stratospheric climatology for O&lt;sub&gt;3&lt;/sub&gt;, H&lt;sub&gt;2&lt;/sub&gt;O, CH&lt;sub&gt;4&lt;/sub&gt;, NO&lt;sub&gt;x&lt;/sub&gt;, HCl and HF derived from HALOE measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-U. Grooß</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>James M. Russell III</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Chemie und Dynamik der Geosphäre I: Stratosphäre (ICG I), Forschungszentrum Jülich, Jülich, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Center for Atmospheric Sciences, Hampton University, Hampton, VA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The Halogen Occultation Experiment (HALOE) on board the Upper
  Atmosphere Research Satellite (UARS) has observed
  mixing ratios of important trace species in the stratosphere for
  more than a decade since 1991.  Here we present a climatology for
  the stratosphere compiled from HALOE  O&lt;sub&gt;3&lt;/sub&gt;, H&lt;sub&gt;2&lt;/sub&gt;O,
  CH&lt;sub&gt;4&lt;/sub&gt;, NO&lt;sub&gt;x&lt;/sub&gt;, HCl, and HF data for the period from 1991 to 2002.
  In this approach, the data
  are averaged over equivalent latitude instead of latitude in order
  to correctly reproduce the gradients at the transport barriers like
  the polar vortex edge. The climatology is compiled for 5 degree
  equivalent latitude bins. Seasonal dependence is taken into
  account by choosing intervals of one month. The climatology is
  available as an electronic supplement.</abstract>
	<references>
	</references>
</article>

