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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-10-17491-2010</article-id>
<title-group>
<article-title>Attribution of stratospheric ozone trends to chemistry and transport: a modelling study</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kiesewetter</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sinnhuber</surname>
<given-names>B.-M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Weber</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Burrows</surname>
<given-names>J. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>07</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>7</issue>
<fpage>17491</fpage>
<lpage>17525</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/10/17491/2010/acpd-10-17491-2010.html">This article is available from http://www.atmos-chem-phys-discuss.net/10/17491/2010/acpd-10-17491-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/10/17491/2010/acpd-10-17491-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/17491/2010/acpd-10-17491-2010.pdf</self-uri>
<abstract>
<p>The decrease of the concentration of ozone depleting substances (ODS) in the
stratosphere over the past decade raises the question to what extent observed
changes in stratospheric ozone over this period are consistent with known
changes in chemical composition and possible changes in atmospheric transport.
Here we present a series of ozone sensitivity calculations with a stratospheric
chemistry transport model (CTM) driven with meteorological reanalyses from the
European Centre for Medium Range Weather Forecast, covering the period
1978–2009. In order to account for the reversal in ODS trends, ozone trends are
analysed in two periods, 1979–1999 and 2000–2009. Effects of ODS changes on the
ozone chemistry are either accounted for or left out, allowing for a distinct
attribution of ozone trends to the different factors of variability, namely ODS
acting via gas phase chemistry, ODS acting via polar heterogeneous chemistry,
and changes in transport and temperature. Modeled column ozone trends are in
excellent agreement with observed trends from the Total Ozone Mapping
Spectrometer (TOMS) and Solar Backscatter UV (SBUV/2) as well as the Global
Ozone Monitoring Experiment (GOME/GOME2) and Scanning Imaging Absorption
Spectrometer for Atmospheric Chartography (SCIAMACHY) instruments. For the
1979–1999 period we find that changes in ODS are the dominant source of the
ozone trend, while changes in transport also contribute signifcantly to the
overall trend. In contrast, for the period 2000–2009 the effect of ODS changes
on total ozone is small. Observed ozone changes can be reproduced well with
the CTM driven with meteorological reanalyses, indicating that the observed
evolution of ozone over the past decade is consistent with our current
understanding of chemistry and transport.</p>
</abstract>
<counts><page-count count="35"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>