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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>5</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-2973-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/2973/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/2973/2005/acpd-5-2973-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/2973/2005/acpd-5-2973-2005.pdf</fulltext_pdf>
	<start_page>2973</start_page>
	<end_page>2988</end_page>
	<publication_date>2005-05-12</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 and CH&lt;sub&gt;4&lt;/sub&gt; derived from HALOE measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-U. Grooß</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. M. Russell III</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut f&amp;uuml;r Chemie und Dynamik der Geosph&amp;auml;re I: Stratosph&amp;auml;re (ICG I), Forschungszentrum J&amp;uuml;lich, J&amp;uuml;lich, Germany</affiliation>
		<affiliation numeration="2" content_type="html">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 over
  more than a decade since 1991.  Here we present a climatology for
  the stratosphere compiled from the HALOE data for ozone, H&lt;sub&gt;2&lt;/sub&gt;O and
  CH&lt;sub&gt;4&lt;/sub&gt; 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. The seasonal dependence is taken into
  account by choosing intervals of one month. The climatology is
  available as an electronic supplement.</abstract>
	<references>
	</references>
</article>

