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<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-4-4489-2004</article-id>
<title-group>
<article-title>Stratospheric age of air computed with trajectories based on various 3-D-Var and 4-D-Var data sets</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Scheele</surname>
<given-names>M. P.</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>Siegmund</surname>
<given-names>P. C.</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. F. J.</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 (KNMI), P.O. Box 201, 3730AE, De Bilt, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>08</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>4</issue>
<fpage>4489</fpage>
<lpage>4506</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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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/4/4489/2004/acpd-4-4489-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/4/4489/2004/acpd-4-4489-2004.pdf</self-uri>
<abstract>
<p>The age of stratospheric air is computed with a trajectory model, using
ECMWF ERA-40 3-D-Var and operational 4-D-Var winds. The sensitivity to the
forecast period and assimilation technique are studied, and the results are
compared with observations and with results from a chemistry transport model
that uses the same data sets. A large number of backward trajectories is
started in the stratosphere, and from the fraction of these trajectories
that has reached the troposphere, the age of air is computed.

&lt;br&gt;&lt;br&gt;
A pilot study in the tropical stratosphere shows that the age increases with
increasing length of the forecast series.

&lt;br&gt;&lt;br&gt;
Next, for three selected data sets (3-D-Var 1-day and 4-D-Var 3-day forecast
series, and 4-D-Var analyses) 5-year backward trajectories are computed that
start all over the globe at an altitude of 20 km. For all data sets the
computed ages of air in the extratropics are smaller than observed. For
4-D-Var forecast series they are closest to the observations, but still
0.5&amp;ndash;1.5 year too small. Compared to the difference in age between the
results for the different data sets, the difference in age between the
trajectory and the chemistry transport model results is small.</p>
</abstract>
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