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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-8-7353-2008</article-id>
<title-group>
<article-title>Using 3DVAR data assimilation system to improve ozone simulations in the Mexico City basin</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bei</surname>
<given-names>N.</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>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>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, La Jolla, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Saint Louis University, Saint Louis, MO, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>12</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>24</issue>
<fpage>7353</fpage>
<lpage>7366</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/8/7353/2008/acp-8-7353-2008.html">This article is available from http://www.atmos-chem-phys.net/8/7353/2008/acp-8-7353-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/7353/2008/acp-8-7353-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/7353/2008/acp-8-7353-2008.pdf</self-uri>
<abstract>
<p>This study investigates the improvement of ozone
(O&lt;sub&gt;3&lt;/sub&gt;) simulations in the Mexico City basin using a
three-dimensional variational (3DVAR) data assimilation system in
meteorological simulations during the MCMA-2003 field measurement campaign.
Meteorological simulations from the NCAR/Penn State mesoscale model (MM5)
are used to drive photochemical simulations with the Comprehensive Air
Quality Model with extensions (CAMx) during a four-day episode on 13–16
April 2003. The simulated wind circulation, temperature, and humidity fields
in the basin with the data assimilation are found to be more consistent with
the observations than those from the reference deterministic forecast. This
leads to improved simulations of plume position, peak O&lt;sub&gt;3&lt;/sub&gt; timing, and
peak O&lt;sub&gt;3&lt;/sub&gt; concentrations in the photochemical model. The improvement in
O&lt;sub&gt;3&lt;/sub&gt; simulations is especially strong during the daytime. The results
demonstrate the importance of applying data assimilation in meteorological
simulations for air quality studies in the Mexico City basin.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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