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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-3-1191-2003</article-id>
<title-group>
<article-title>Out of Africa: High aerosol concentrations in the upper troposphere over Africa</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heintzenberg</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>Hermann</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>Theiss</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Leibniz-Institute for Tropospheric Research, Permoserstr. 15, 04318 Leipzig, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>08</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>4</issue>
<fpage>1191</fpage>
<lpage>1198</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2003 J. Heintzenberg et al.</copyright-statement>
<copyright-year>2003</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/3/1191/2003/acp-3-1191-2003.html">This article is available from https://acp.copernicus.org/articles/3/1191/2003/acp-3-1191-2003.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/3/1191/2003/acp-3-1191-2003.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/3/1191/2003/acp-3-1191-2003.pdf</self-uri>
<abstract>
<p>In the year 2000, six flights (three southbound and three northbound) of the CARIBIC project
      were conducted between Germany and two destinations in the southern hemisphere
      (Windhoek, Namibia and Cape Town, South Africa).  In the present report, results on particle
      number concentrations are discussed in three size ranges (&amp;gt;4 nm, &amp;gt;12
      nm, and &amp;gt;18 nm particle diameter) during the unique transequatorial Africa flights.  The flights covered a total
      of about 80 h in May, July, and December.  Thus, no claim can be made for long-term
      representativeness of the aerosol data.  Nevertheless, they are the first upper systematic
      tropospheric transequatorial aerosol profiles over Africa.  The average aerosol results show a
      broad maximum, roughly symmetrical to the equator, which compares well in latitudinal
      extent to a maximum of CO concentrations measured on the same flights.  This export of
      continental surface aerosol to the upper troposphere will be dispersed on a global scale both
      with the easterly flow near the equator and with the westerlies in the adjacent subtropical
      regions.  There was strong evidence of recent new particle formation before aerosol arrival at
      flight level, in particular during the time periods between 9:00 and 13:00 local time over
      Africa.  Direct and indirect climate effects of the respective particulate matter remain to be
      investigated by future flights with the ongoing extension of the CARIBIC payload towards
      size-resolved measurements above 100 nm particle diameter.  At the same time global
      chemical transport models and aerosol dynamics models need to be extended to be able to
      reproduce the CARIBIC findings over Africa.</p>
</abstract>
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