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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-3-447-2003</article-id>
<title-group>
<article-title>On the use of mass-conserving wind fields in chemistry-transport models</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bregman</surname>
<given-names>B.</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>Segers</surname>
<given-names>A.</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>Krol</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Meijer</surname>
<given-names>E.</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>van Velthoven</surname>
<given-names>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>Royal Netherlands Meteorological Institute, P.O. Box 201, 3730 AE, De Bilt, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Marine and Atmospheric Research Utrecht, Princetonplein 5, 3584 CC, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>04</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>2</issue>
<fpage>447</fpage>
<lpage>457</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.net/3/447/2003/acp-3-447-2003.html">This article is available from http://www.atmos-chem-phys.net/3/447/2003/acp-3-447-2003.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/3/447/2003/acp-3-447-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/3/447/2003/acp-3-447-2003.pdf</self-uri>
<abstract>
<p>A new method has been developed that provides mass-conserving wind fields for
      global chemistry-transport models. In previous global Eulerian modeling studies a mass-imbalance was found between the model mass transport and the
      surface pressure tendencies. Several methods have been suggested to correct
      for this imbalance, but so far no satisfactory solution has been found. Our
      new method solves these problems by using the wind fields in a spherical harmonical form (divergence and vorticity) by mimicing the physics of the
      weather forecast model as closely as possible. A 3-D chemistry-transport model
      was used to show that the calculated ozone fields with the new processing method agree remarkably better with ozone observations in the upper
      troposphere and lower stratosphere. In addition, the calculated age of air in
      the lower stratosphere show better agreement with observations, although the
      air remains still too young in the extra-tropical stratosphere.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
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