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	<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>8</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-565-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/565/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/565/2008/acp-8-565-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/565/2008/acp-8-565-2008.pdf</fulltext_pdf>
	<start_page>565</start_page>
	<end_page>578</end_page>
	<publication_date>2008-02-07</publication_date>
	<article_title content_type="html">The impact of transport across the polar vortex edge on Match ozone loss estimates</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-U. Grooß</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Müller</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. Konopka</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H.-M. Steinhorst</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. Engel</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>T. Möbius</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>C. M. Volk</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Forschungszentrum Jülich, Institut für Chemie und Dynamik der Geosphäre, ICG-1: Stratosphäre, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Johann Wolfgang Goethe-Universität, Frankfurt, Institut für Atmosphäre und Umwelt, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The Match method for the quantification of polar chemical ozone loss
  is investigated mainly with respect to the impact of the transport
  of air masses across the vortex edge.
  For the winter 2002/03, we show that significant transport across
  the vortex edge occurred and was simulated by the Chemical
  Lagrangian Model of the Stratosphere.  In-situ observations of inert
  tracers and ozone from HAGAR on the Geophysica aircraft and
  balloon-borne sondes, and remote observations from MIPAS on the
  ENVISAT satellite were reproduced well by CLaMS.  The model even
  reproduced a small vortex remnant that remained a distinct feature
  until June 2003 and was also observed in-situ by a balloon-borne
  whole air sampler.
  We use this CLaMS simulation to quantify the impact of transport
  across the vortex edge on ozone loss estimates from the Match method.
  We show that a time integration of the determined vortex average
  ozone loss rates, as performed in Match, results in a larger ozone loss
  than the polar vortex average ozone loss in CLaMS.
  The determination of the Match ozone loss rates is also influenced
  by the transport of air across the vortex edge. We use  the model
  to investigate how the sampling of the ozone sondes on which Match
  is based represents the vortex average ozone loss rate.
  Both the time integration of ozone loss and the determination of
  ozone loss rates for Match are evaluated using the winter 2002/2003
  CLaMS simulation.  These impacts can explain the majority of the
  differences between CLaMS and Match column ozone loss.
  While the investigated effects somewhat reduce the apparent
  discrepancy in January ozone loss rates reported earlier, a distinct
  discrepancy between simulations and Match remains. However, its
  contribution to the accumulated ozone loss over the winter is not
  large.</abstract>
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</article>

