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<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-6-7959-2006</article-id>
<title-group>
<article-title>Characterizing ozone production in the Mexico City Metropolitan Area: a case study using a chemical transport model</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>
</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="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>
</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="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>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>Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, MA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Molina Center for Energy and the Environment, CA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Department of Chemistry and Biochemistry, University of California, San Diego, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>08</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>4</issue>
<fpage>7959</fpage>
<lpage>8009</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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<abstract>
<p>An episodic simulation is conducted to characterize ozone (O&lt;sub&gt;3&lt;/sub&gt;)
photochemical production and investigate its sensitivity to emission changes
of ozone precursors in the Mexico City Metropolitan Area (MCMA) using the
Comprehensive Air Quality Model with extensions (CAMx). High O&lt;sub&gt;x&lt;/sub&gt;
(O&lt;sub&gt;3&lt;/sub&gt;+NO&lt;sub&gt;2&lt;/sub&gt;) photochemical production rates of 10&amp;ndash;80 ppb/h are
predicted due to the high reactivity of volatile organic compounds (VOCs) in
which alkanes, alkenes, and aromatics exert comparable contributions. The
predicted ozone production efficiency is between 4&amp;ndash;10 O&lt;sub&gt;3&lt;/sub&gt; molecules per
NO&lt;sub&gt;x&lt;/sub&gt; molecule oxidized, and increases with VOC-to-NO&lt;sub&gt;2&lt;/sub&gt; reactivity
ratio. Process apportionment analyses indicate significant outflow of
pollutants such as O&lt;sub&gt;3&lt;/sub&gt; and peroxyacetyl nitrate (PAN) from the urban
area to the surrounding regional environment. PAN is not in chemical-thermal
equilibrium during the photochemically active periods. Sensitivity studies
of O&lt;sub&gt;3&lt;/sub&gt; production suggest that O&lt;sub&gt;3&lt;/sub&gt; formation in the MCMA urban
region with less chemical aging (NO&lt;sub&gt;z&lt;/sub&gt;/NO&lt;sub&gt;y&lt;/sub&gt;&amp;lt;0.3) is VOC-limited.
Both the simulated behavior of O&lt;sub&gt;3&lt;/sub&gt; production and its sensitivities to
precursors suggest that midday O&lt;sub&gt;3&lt;/sub&gt; formation during this episode is VOC
sensitive in the urban region on the basis of the current emissions
inventory. More episodic studies are needed to construct a comprehensive and
representative picture of the O&lt;sub&gt;3&lt;/sub&gt; production characteristics and its
response to emission controls.</p>
</abstract>
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