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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-7-2165-2007</article-id>
<title-group>
<article-title>A chemistry-transport model simulation of middle atmospheric ozone from 1980 to 2019 using coupled chemistry GCM winds and temperatures</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Damski</surname>
<given-names>J.</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>Thölix</surname>
<given-names>L.</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>Backman</surname>
<given-names>L.</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>Kaurola</surname>
<given-names>J.</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>Taalas</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Austin</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Butchart</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Research and Development, Finnish Meteorological Institute, P.O.Box 503, FI-00101 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Regional and Technical Cooperation for Development Department (RCD), World Meteorological Organization,  case Postale 2300, CH-1211 Genève 2, Switzerland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Geophysical fluid dynamics Laboratory, Princeton, NJ, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Climate Research Division, Met Office, Exeter, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Physical Sciences, University of Helsinki, P.O.Box 64, FI-00014 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>05</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>9</issue>
<fpage>2165</fpage>
<lpage>2181</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>
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<abstract>
<p>A global 40-year simulation from 1980 to 2019 was performed with the
  FinROSE chemistry-transport model based on the use of coupled
  chemistry GCM-data. The main focus of our analysis is on
  climatological-scale processes in high latitudes. The resulting
  trend estimates for the past period (1980&amp;ndash;1999) agree well with
  observation-based trend estimates. The results for the future period
  (2000&amp;ndash;2019) suggest that the extent of seasonal ozone depletion over both
  northern and southern high-latitudes has likely reached its maximum.
  Furthermore, while climate change is expected to cool the stratosphere,
  this cooling is unlikely to accelerate significantly high latitude ozone
  depletion. However, the recovery of seasonal high latitude ozone
  losses will not take place during the next 15 years.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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