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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-8-7571-2008</article-id>
<title-group>
<article-title>Characterizing ozone production and response under different meteorological conditions in Mexico City</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lei</surname>
<given-names>W.</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>Zavala</surname>
<given-names>M.</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>de Foy</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Volkamer</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Molina</surname>
<given-names>L. T.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Molina Center for Energy and the Environment, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, MA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Earth and Atmospheric Sciences, Saint Louis University, MO, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Chemistry and Biochemistry, University of Colorado at Boulder, CO, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>12</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>24</issue>
<fpage>7571</fpage>
<lpage>7581</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/8/7571/2008/acp-8-7571-2008.html">This article is available from http://www.atmos-chem-phys.net/8/7571/2008/acp-8-7571-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/7571/2008/acp-8-7571-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/7571/2008/acp-8-7571-2008.pdf</self-uri>
<abstract>
<p>Photochemistry in polluted atmospheres, particularly the formation of ozone
(O&lt;sub&gt;3&lt;/sub&gt;), depends not only on pollutant emissions, but also on
meteorological conditions. In this study a 3-D chemical transport model CAMx
was employed to investigate the O&lt;sub&gt;3&lt;/sub&gt; formation and its response to
emissions reduction under three distinctively different meteorological
conditions in the Mexico City Metropolitan Area during the MCMA-2003 field
measurement campaign. The O&lt;sub&gt;3&lt;/sub&gt; formation characteristics and sensitivity
to emissions change were found to be weakly dependent on the meteorological
conditions. The evolution of O&lt;sub&gt;3&lt;/sub&gt; formation and its sensitivity to
NO&lt;sub&gt;x&lt;/sub&gt; and VOC levels were also examined along the photochemical plume
transport pathway. The midday O&lt;sub&gt;3&lt;/sub&gt; production was found to undergo a
rapid increase in a narrow range of chemical aging, while downwind plumes
were characterized with low and constant O&lt;sub&gt;3&lt;/sub&gt; production, and plumes
along their transport pathway were characterized by a combination of the
two. The O&lt;sub&gt;3&lt;/sub&gt; formation was more VOC sensitive near the source area, but
as the plume became chemically aged, O&lt;sub&gt;3&lt;/sub&gt; formation became progressively
VOC insensitive and more NO&lt;sub&gt;x&lt;/sub&gt; sensitive.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>