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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-10-2079-2010</article-id>
<title-group>
<article-title>MAX-DOAS measurements in southern China: retrieval of aerosol extinctions and validation using ground-based in-situ data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Li</surname>
<given-names>X.</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>Brauers</surname>
<given-names>T.</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>Shao</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>Garland</surname>
<given-names>R. M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wagner</surname>
<given-names>T.</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>Deutschmann</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wahner</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>College of Environmental Sciences and Engineering, Peking University, Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Chemistry and Dynamics of the Geosphere (ICG-2), Forschungszentrum Jülich, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Satellite Group, Max Planck Institute for Chemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Institute for Environmental Physics, Universität Heidelberg, Heidelberg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>03</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>5</issue>
<fpage>2079</fpage>
<lpage>2089</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/10/2079/2010/acp-10-2079-2010.html">This article is available from http://www.atmos-chem-phys.net/10/2079/2010/acp-10-2079-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/2079/2010/acp-10-2079-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/2079/2010/acp-10-2079-2010.pdf</self-uri>
<abstract>
<p>We performed MAX-DOAS measurements during the PRiDe-PRD2006 campaign
in the Pearl River Delta region 50 km north of Guangzhou, China, for 4 weeks
in June 2006. We used an instrument sampling at 7 different elevation angles
between 3&amp;deg; and 90&amp;deg;. During 9 cloud-free days, differential slant
column densities (DSCDs) of O&lt;sub&gt;4&lt;/sub&gt; (O&lt;sub&gt;2&lt;/sub&gt; dimer) absorptions between
351 nm and 389 nm were evaluated for 6 elevation angles. Here, we show
that radiative transfer modeling of the DSCDS can be used to retrieve the
aerosol extinction and the height of the boundary layer. A comparison of the
aerosol extinction with simultaneously recorded, ground based nephelometer
data shows excellent agreement.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>