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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-9-24629-2009</article-id>
<title-group>
<article-title>Temporal variation of elemental carbon in Guangzhou, China, in summer 2006</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Verma</surname>
<given-names>R. L.</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>Sahu</surname>
<given-names>L. K.</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>Kondo</surname>
<given-names>Y.</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>Takegawa</surname>
<given-names>N.</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>Han</surname>
<given-names>S.</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>Jung</surname>
<given-names>J. S.</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>Kim</surname>
<given-names>Y. J.</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>Fan</surname>
<given-names>S.</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>Sugimoto</surname>
<given-names>N.</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>Shammaa</surname>
<given-names>M. H.</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>Zhang</surname>
<given-names>Y. H.</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>Zhao</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Research Center for Advanced Science and Technology, University of Tokyo, Tokyo, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Advanced Environmental Monitoring Research Center, Department of Environmental Science and Engineering, Gwangju Institute of Science and Technology (GIST), Gwangju, Republic of Korea</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Environmental Meteorology, School of Environmental Science and Engineering, Sun Yat-sen University, Guangzhou, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Atmospheric Remote Sensing Section, National Institute for Environmental Studies, Tsukuba, Japan</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental  Science and Engineering, Peking University, Beijing, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Air Quality Research Center, University of California, Davis, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>6</issue>
<fpage>24629</fpage>
<lpage>24667</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/9/24629/2009/acpd-9-24629-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/24629/2009/acpd-9-24629-2009.pdf</self-uri>
<abstract>
<p>In situ measurements of the mass concentration of elemental carbon (EC) and mixing ratios of
carbon monoxide (CO) and carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) were made at Guangzhou, an
urban measurement site in the Pearl River Delta (PRD), China, in July 2006. The average&amp;plusmn;standard deviation (SD) concentrations of EC, CO, and CO&lt;sub&gt;2&lt;/sub&gt; were
4.7&amp;plusmn;2.3 &amp;mu;g C m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, 798&amp;plusmn;459 ppbv and
400&amp;plusmn;13 ppmv, respectively. The trends of these species were mainly controlled
by synoptic-scale changes in meteorology during the campaign. Based on back trajectories,
data are analyzed separately for two different air mass types representing northerly and
southerly flows. Northerly air masses, constituting about 25% of the campaign, were
mainly impacted by stagnant conditions, resulting in elevated levels of pollutants. On the
other hand, southerly air masses measured during most of the campaign were mostly influenced
by clean marine air. The diurnal patterns of EC, CO, and CO&lt;sub&gt;2&lt;/sub&gt; exhibited peak
concentrations during the morning and evening hours coinciding with rush-hour traffic. The
diurnal variations of EC and &amp;Delta;EC/&amp;Delta;CO closely followed the
traffic pattern of heavy-duty vehicles (HDV) in Guangzhou, similar to that observed in
Beijing. The level of EC in this campaign was similar to values reported during previous
studies at other sites surrounding Guangzhou. The average slopes of &amp;Delta;EC/&amp;Delta;CO, &amp;Delta;EC/&amp;Delta;CO&lt;sub&gt;2&lt;/sub&gt;, 
and &amp;Delta;CO/&amp;Delta;CO&lt;sub&gt;2&lt;/sub&gt; were 0.0054 &amp;mu;g C m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;/ppbv, 0.15 &amp;mu;g C m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;/ppmv, 
and 46.4 ppbv/ppmv, respectively, agreeing reasonably well with
their respective emission ratios derived from regional emission inventories.</p>
</abstract>
<counts><page-count count="39"/></counts>
</article-meta>
</front>
<body/>
<back>
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