<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<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-3-2661-2003</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>19</day>
<month>05</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>3</issue>
<fpage>2661</fpage>
<lpage>2689</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/3/2661/2003/acpd-3-2661-2003.html">This article is available from http://www.atmos-chem-phys-discuss.net/3/2661/2003/acpd-3-2661-2003.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/3/2661/2003/acpd-3-2661-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/3/2661/2003/acpd-3-2661-2003.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>
<counts><page-count count="29"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>